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id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Mike Kendall</h3></div><div class="js-work-strip profile--work_container" data-work-id="113721032"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/113721032/Seawater_carbonate_chemistry_and_biological_processes_during_experiments_with_postlarvae_of_barnacle_of_Semibalanus_balanoides_and_Elminius_modestus_2010"><img alt="Research paper thumbnail of Seawater carbonate chemistry and biological processes during experiments with postlarvae of barnacle of Semibalanus balanoides and Elminius modestus, 2010" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/113721032/Seawater_carbonate_chemistry_and_biological_processes_during_experiments_with_postlarvae_of_barnacle_of_Semibalanus_balanoides_and_Elminius_modestus_2010">Seawater carbonate chemistry and biological processes during experiments with postlarvae of barnacle of Semibalanus balanoides and Elminius modestus, 2010</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Ocean acidification and global warming are occurring concomitantly, yet few studies have investig...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Ocean acidification and global warming are occurring concomitantly, yet few studies have investigated how organisms will respond to increases in both temperature and CO2. Intertidal microcosms were used to examine growth, shell mineralogy and survival of two intertidal barnacle post-larvae, Semibalanus balanoides and Elminius modestus, at two temperatures (14 and 19掳C) and two CO2 concentrations (380 and 1,000 ppm), fed with a mixed diatom-flagellate diet at 15,000 cells ml-1 with flow rate of 10 ml-1 min-1. Control growth rates, using operculum diameter, were 14 卤 8 碌m day-1 and 6 卤 2 碌m day-1 for S. balanoides and E. modestus, respectively. Subtle, but significant decreases in E. modestus growth rate were observed in high CO2 but there were no impacts on shell calcium content and survival by either elevated temperature or CO2. S. balanoides exhibited no clear alterations in growth rate but did show a large reduction in shell calcium content and survival under elevated temperature and CO2. These results suggest that a decrease by 0.4 pH(NBS) units alone would not be sufficient to directly impact the survival of barnacles during the first month post-settlement. However, in conjunction with a 4-5掳C increase in temperature, it appears that significant changes to the biology of these organisms will ensue.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="113721032"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="113721032"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 113721032; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=113721032]").text(description); $(".js-view-count[data-work-id=113721032]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 113721032; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='113721032']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 113721032, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=113721032]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":113721032,"title":"Seawater carbonate chemistry and biological processes during experiments with postlarvae of barnacle of Semibalanus balanoides and Elminius modestus, 2010","translated_title":"","metadata":{"abstract":"Ocean acidification and global warming are occurring concomitantly, yet few studies have investigated how organisms will respond to increases in both temperature and CO2. 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These results suggest that a decrease by 0.4 pH(NBS) units alone would not be sufficient to directly impact the survival of barnacles during the first month post-settlement. However, in conjunction with a 4-5掳C increase in temperature, it appears that significant changes to the biology of these organisms will ensue.","publication_date":{"day":29,"month":3,"year":2010,"errors":{}}},"translated_abstract":"Ocean acidification and global warming are occurring concomitantly, yet few studies have investigated how organisms will respond to increases in both temperature and CO2. Intertidal microcosms were used to examine growth, shell mineralogy and survival of two intertidal barnacle post-larvae, Semibalanus balanoides and Elminius modestus, at two temperatures (14 and 19掳C) and two CO2 concentrations (380 and 1,000 ppm), fed with a mixed diatom-flagellate diet at 15,000 cells ml-1 with flow rate of 10 ml-1 min-1. Control growth rates, using operculum diameter, were 14 卤 8 碌m day-1 and 6 卤 2 碌m day-1 for S. balanoides and E. modestus, respectively. Subtle, but significant decreases in E. modestus growth rate were observed in high CO2 but there were no impacts on shell calcium content and survival by either elevated temperature or CO2. S. balanoides exhibited no clear alterations in growth rate but did show a large reduction in shell calcium content and survival under elevated temperature and CO2. These results suggest that a decrease by 0.4 pH(NBS) units alone would not be sufficient to directly impact the survival of barnacles during the first month post-settlement. 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Model parameters and equations</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Model parameters and equations.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="113721031"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="113721031"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 113721031; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=113721031]").text(description); $(".js-view-count[data-work-id=113721031]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 113721031; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='113721031']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 113721031, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=113721031]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":113721031,"title":"Appendix B. 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Comeau, S, Gorsky, G, Jeffree, R, Teyssle, JL and Gattuso, JP. 2009. Impact of ocean ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">... 200912. Comeau, S, Gorsky, G, Jeffree, R, Teyssle, JL and Gattuso, JP. 2009. Impact of ocean acidification on a key Arctic pelagic mollusc (Limacina helicina). Biogeosciences , 6: 1877聳82. ... 200912. 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window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=62438260]").text(description); $(".js-view-count[data-work-id=62438260]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 62438260; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='62438260']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 62438260, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2cae0543d2d0ec0522926c875d47b655" } } $('.js-work-strip[data-work-id=62438260]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":62438260,"title":"Calcification, a physiological process to be considered in the context of the whole organism","translated_title":"","metadata":{"publisher":"Copernicus GmbH","grobid_abstract":"Marine organisms that produce calcium carbonate structures are predicted to be most vulnerable to a decline in oceanic pH (ocean acidification) based on the understanding that calcification rates will decrease as a result of changes in the seawater carbonate chemistry thereby reducing carbonate ion concentration (and associated saturation states). Coastal seas are critical components of the global carbon cycle yet little research has been conducted on acidification impacts on coastal benthic organisms. Here, a critical appraisal of calcification in six benthic species showed, contrary to popular predictions, calcification can increase, and not decrease, in acidified seawater. Measuring the changes in calcium in isolated calcium carbonate structure as well as structures from live animals exposed to acidified seawater allowed a comparison between a species' ability to calcify and the dissolution affects across decreasing levels of pH. Calcium carbonate production is dependant on the ability to increase calcification thus counteracting an increase in dissolution. Comparison with paleoecological studies of past high carbon dioxide (CO 2) events presents a similar picture. This conclusion implies that calcification may not be the critical process impacted by ocean acidification; particularly as all species investigated displayed physiological trade offs including reduced metabolism, health, and behavioural responses, in association with this calcification upregulation, which possess as great a threat to survival as an inability to calcify.","publication_name":"Biogeosciences Discussions","grobid_abstract_attachment_id":75203021},"translated_abstract":null,"internal_url":"https://www.academia.edu/62438260/Calcification_a_physiological_process_to_be_considered_in_the_context_of_the_whole_organism","translated_internal_url":"","created_at":"2021-11-26T01:28:28.118-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":90363891,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":75203021,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/75203021/thumbnails/1.jpg","file_name":"Calcification_a_physiological_process_to20211126-28945-1frveaq.pdf","download_url":"https://www.academia.edu/attachments/75203021/download_file?st=MTczMjk4MTIwOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Calcification_a_physiological_process_to.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/75203021/Calcification_a_physiological_process_to20211126-28945-1frveaq.pdf?1637918976=\u0026response-content-disposition=attachment%3B+filename%3DCalcification_a_physiological_process_to.pdf\u0026Expires=1732978495\u0026Signature=Zt2FusJ1nEKjfAPHivROoHotAQE-z-IR47RHv5YyxbE~V0dAsJNpDyskszrIJtrM3GOjpX0yGy~r8TV-Bt-JAvCwbA6N2BOa0DqlNS~zga4ID0vUPQA-~gqBBooA9gk7oaYm0sEwRy6J4hRv2Z4sLcve6zWOsIPY7xhfyGWvInvIU3vYqTGNXUdbvJYfH67POJTLnOhfkly3QwfBweIY7zCO6hEmDPyKsrtchaQj4DtQzeM1HWmI4OSl3a8sYx~nmDZ6P2euI5~KdLPtctIFRvYJ4zTivz~7RSZf6Ur0pKAE8rXMNlGDTu~Iyk~x6DtT1hTA46MV86tvkIKuKCNQUw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Calcification_a_physiological_process_to_be_considered_in_the_context_of_the_whole_organism","translated_slug":"","page_count":18,"language":"en","content_type":"Work","owner":{"id":90363891,"first_name":"Mike","middle_initials":null,"last_name":"Kendall","page_name":"MikeKendall6","domain_name":"independent","created_at":"2018-09-07T05:51:20.536-07:00","display_name":"Mike Kendall","url":"https://independent.academia.edu/MikeKendall6"},"attachments":[{"id":75203021,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/75203021/thumbnails/1.jpg","file_name":"Calcification_a_physiological_process_to20211126-28945-1frveaq.pdf","download_url":"https://www.academia.edu/attachments/75203021/download_file?st=MTczMjk4MTIwOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Calcification_a_physiological_process_to.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/75203021/Calcification_a_physiological_process_to20211126-28945-1frveaq.pdf?1637918976=\u0026response-content-disposition=attachment%3B+filename%3DCalcification_a_physiological_process_to.pdf\u0026Expires=1732978495\u0026Signature=Zt2FusJ1nEKjfAPHivROoHotAQE-z-IR47RHv5YyxbE~V0dAsJNpDyskszrIJtrM3GOjpX0yGy~r8TV-Bt-JAvCwbA6N2BOa0DqlNS~zga4ID0vUPQA-~gqBBooA9gk7oaYm0sEwRy6J4hRv2Z4sLcve6zWOsIPY7xhfyGWvInvIU3vYqTGNXUdbvJYfH67POJTLnOhfkly3QwfBweIY7zCO6hEmDPyKsrtchaQj4DtQzeM1HWmI4OSl3a8sYx~nmDZ6P2euI5~KdLPtctIFRvYJ4zTivz~7RSZf6Ur0pKAE8rXMNlGDTu~Iyk~x6DtT1hTA46MV86tvkIKuKCNQUw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":68527,"name":"Ocean acidification","url":"https://www.academia.edu/Documents/in/Ocean_acidification"},{"id":82100,"name":"Global Carbon Cycle","url":"https://www.academia.edu/Documents/in/Global_Carbon_Cycle"},{"id":151321,"name":"Biogeosciences","url":"https://www.academia.edu/Documents/in/Biogeosciences"}],"urls":[{"id":14504512,"url":"http://www.biogeosciences-discuss.net/6/2267/2009/bgd-6-2267-2009.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="62438259"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/62438259/The_stability_of_the_deposit_feeding_community_of_a_mud_flat_in_the_River_Tees"><img alt="Research paper thumbnail of The stability of the deposit feeding community of a mud flat in the River Tees" class="work-thumbnail" src="https://attachments.academia-assets.com/75203010/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/62438259/The_stability_of_the_deposit_feeding_community_of_a_mud_flat_in_the_River_Tees">The stability of the deposit feeding community of a mud flat in the River Tees</a></div><div class="wp-workCard_item"><span>Estuarine and Coastal Marine Science</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="42a2308aedab587806271b91cba8ea39" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":75203010,"asset_id":62438259,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/75203010/download_file?st=MTczMjk4MTIwOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="62438259"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="62438259"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 62438259; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=62438259]").text(description); $(".js-view-count[data-work-id=62438259]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 62438259; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='62438259']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 62438259, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="62438255"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/62438255/Variations_in_some_morphological_characteristics_of_Polydora_ciliata_Johnston_"><img alt="Research paper thumbnail of Variations in some morphological characteristics of Polydora ciliata (Johnston)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/62438255/Variations_in_some_morphological_characteristics_of_Polydora_ciliata_Johnston_">Variations in some morphological characteristics of Polydora ciliata (Johnston)</a></div><div class="wp-workCard_item"><span>Http Dx Doi Org 10 1080 00222938000770351</span><span>, Feb 17, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT On investigation of a dense population of mud tube building polychaetes tentatively iden...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT On investigation of a dense population of mud tube building polychaetes tentatively identified as Polydora ciliata it was found that many individuals also showed morphological characteristics more usually associated with other members of the same genus. This prompted the examination of the morphology of P. ciliata from a number of different areas with the aim of assessing the stability of some of the characters used in the taxonomy of its genus. These proved to be highly variable, did not group together consistently and overlapped with some of those of P. limicola (Annenkova) and P. ligni Webster. No clear distinction between P. ciliata and P. limicola could be made on the grounds of the characteristics examined but the overlap between P. ciliata and P. ligni was small.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="62438255"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="62438255"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 62438255; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=62438255]").text(description); $(".js-view-count[data-work-id=62438255]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 62438255; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='62438255']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 62438255, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=62438255]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":62438255,"title":"Variations in some morphological characteristics of Polydora ciliata (Johnston)","translated_title":"","metadata":{"abstract":"ABSTRACT On investigation of a dense population of mud tube building polychaetes tentatively identified as Polydora ciliata it was found that many individuals also showed morphological characteristics more usually associated with other members of the same genus. This prompted the examination of the morphology of P. ciliata from a number of different areas with the aim of assessing the stability of some of the characters used in the taxonomy of its genus. These proved to be highly variable, did not group together consistently and overlapped with some of those of P. limicola (Annenkova) and P. ligni Webster. No clear distinction between P. ciliata and P. limicola could be made on the grounds of the characteristics examined but the overlap between P. ciliata and P. ligni was small.","publication_date":{"day":17,"month":2,"year":2007,"errors":{}},"publication_name":"Http Dx Doi Org 10 1080 00222938000770351"},"translated_abstract":"ABSTRACT On investigation of a dense population of mud tube building polychaetes tentatively identified as Polydora ciliata it was found that many individuals also showed morphological characteristics more usually associated with other members of the same genus. This prompted the examination of the morphology of P. ciliata from a number of different areas with the aim of assessing the stability of some of the characters used in the taxonomy of its genus. These proved to be highly variable, did not group together consistently and overlapped with some of those of P. limicola (Annenkova) and P. ligni Webster. No clear distinction between P. ciliata and P. limicola could be made on the grounds of the characteristics examined but the overlap between P. ciliata and P. ligni was small.","internal_url":"https://www.academia.edu/62438255/Variations_in_some_morphological_characteristics_of_Polydora_ciliata_Johnston_","translated_internal_url":"","created_at":"2021-11-26T01:28:27.488-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":90363891,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Variations_in_some_morphological_characteristics_of_Polydora_ciliata_Johnston_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":90363891,"first_name":"Mike","middle_initials":null,"last_name":"Kendall","page_name":"MikeKendall6","domain_name":"independent","created_at":"2018-09-07T05:51:20.536-07:00","display_name":"Mike Kendall","url":"https://independent.academia.edu/MikeKendall6"},"attachments":[],"research_interests":[{"id":155,"name":"Evolutionary Biology","url":"https://www.academia.edu/Documents/in/Evolutionary_Biology"},{"id":173,"name":"Zoology","url":"https://www.academia.edu/Documents/in/Zoology"},{"id":9588,"name":"Natural History","url":"https://www.academia.edu/Documents/in/Natural_History"}],"urls":[{"id":14504508,"url":"http://www.tandfonline.com/doi/abs/10.1080/00222938000770351?journalCode=tnah20"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="62438254"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/62438254/Can_ocean_acidification_affect_population_dynamics_of_the_barnacle_Semibalanus_balanoides_at_its_southern_range_edge"><img alt="Research paper thumbnail of Can ocean acidification affect population dynamics of the barnacle Semibalanus balanoides at its southern range edge?" class="work-thumbnail" src="https://attachments.academia-assets.com/75203016/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/62438254/Can_ocean_acidification_affect_population_dynamics_of_the_barnacle_Semibalanus_balanoides_at_its_southern_range_edge">Can ocean acidification affect population dynamics of the barnacle Semibalanus balanoides at its southern range edge?</a></div><div class="wp-workCard_item"><span>Http Dx Doi Org 10 1890 09 1987 1</span><span>, Oct 1, 2010</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a7efa224c2cd082e82d5aa994a342923" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":75203016,"asset_id":62438254,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/75203016/download_file?st=MTczMjk4MTIwOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="62438254"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="62438254"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 62438254; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=62438254]").text(description); $(".js-view-count[data-work-id=62438254]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 62438254; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='62438254']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 62438254, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "a7efa224c2cd082e82d5aa994a342923" } } $('.js-work-strip[data-work-id=62438254]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":62438254,"title":"Can ocean acidification affect population dynamics of the barnacle Semibalanus balanoides at its southern range edge?","translated_title":"","metadata":{"grobid_abstract":"The global ocean and atmosphere are warming. There is increasing evidence suggesting that, in addition to other environmental factors, climate change is affecting species distributions and local population dynamics. Additionally, as a consequence of the growing levels of atmospheric carbon dioxide (CO 2), the oceans are taking up increasing amounts of this CO 2 , causing ocean pH to decrease (ocean acidification). The relative impacts of ocean acidification on population dynamics have yet to be investigated, despite many studies indicating that there will be at least a sublethal impact on many marine organisms, particularly key calcifying organisms. Using empirical data, we forced a barnacle (Semibalanus balanoides) population model to investigate the relative influence of sea surface temperature (SST) and ocean acidification on a population nearing the southern limit of its geographic distribution. Hindcast models were compared to observational data from Cellar Beach (southwestern United Kingdom). Results indicate that a declining pH trend (脌0.0017 unit/yr), indicative of ocean acidification over the past 50 years, does not cause an observable impact on the population abundance relative to changes caused by fluctuations in temperature. Below the critical temperature (here T crit 录 13.18C), pH has a more significant affect on population dynamics at this southern range edge. However, above this value, SST has the overriding influence. At lower SST, a decrease in pH (according to the National Bureau of Standards, pH NBS) from 8.2 to 7.8 can significantly decrease the population abundance. The lethal impacts of ocean acidification observed in experiments on early life stages reduce cumulative survival by ;25%, which again will significantly alter the population level at this southern limit. 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href="https://www.academia.edu/62438253/Effects_of_bottom_trawling_on_ecosystem_functioning"><img alt="Research paper thumbnail of Effects of bottom trawling on ecosystem functioning" class="work-thumbnail" src="https://attachments.academia-assets.com/75203381/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/62438253/Effects_of_bottom_trawling_on_ecosystem_functioning">Effects of bottom trawling on ecosystem functioning</a></div><div class="wp-workCard_item"><span>Journal of Experimental Marine Biology and Ecology</span><span>, Nov 1, 2008</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="407ecfa75b61ff67d1d161cc7c5c4b35" class="wp-workCard--action" rel="nofollow" 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observations with data from controlled mesocosm experiments this study demonstrated that bottom trawling has the potential to cause long-term impacts on sediment nutrient fluxes. Field observations confirmed that trawling reduced the density of important bioturbators in the study area, but revealed only weak effects of trawling on nutrient fluxes. The importance of the decline in bioturbators was demonstrated in the mesocosm experiments where the density of four key bioturbators (Brissopsis lyrifera, Nuculana minuta, Calocaris macandreae and Amphiura chiajei) showed significant correlations with nutrient flux. All four species caused an increase in the rate at which silicate was released from the sediment, but their effect on nitrogen cycling were species specific. Bioturbators that bulldoze through the sediment (B. lyrifera and N. minuta) increased the loss of dissolved inorganic nitrogen (DIN) from the sediment, whereas those that irrigate burrows within the sediment (C. macandreae and A. chiajei) caused increased uptake of DIN. This shows that the activities of the species present can determine whether the seabed acts as a source or a sink of nitrogen nutrients. By combining these experimental results with field observations of bioturbator abundances, we demonstrate the potential impacts of trawling on benthic ecosystem function. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="11093133" id="papers"><div class="js-work-strip profile--work_container" data-work-id="113721032"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/113721032/Seawater_carbonate_chemistry_and_biological_processes_during_experiments_with_postlarvae_of_barnacle_of_Semibalanus_balanoides_and_Elminius_modestus_2010"><img alt="Research paper thumbnail of Seawater carbonate chemistry and biological processes during experiments with postlarvae of barnacle of Semibalanus balanoides and Elminius modestus, 2010" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/113721032/Seawater_carbonate_chemistry_and_biological_processes_during_experiments_with_postlarvae_of_barnacle_of_Semibalanus_balanoides_and_Elminius_modestus_2010">Seawater carbonate chemistry and biological processes during experiments with postlarvae of barnacle of Semibalanus balanoides and Elminius modestus, 2010</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Ocean acidification and global warming are occurring concomitantly, yet few studies have investig...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Ocean acidification and global warming are occurring concomitantly, yet few studies have investigated how organisms will respond to increases in both temperature and CO2. Intertidal microcosms were used to examine growth, shell mineralogy and survival of two intertidal barnacle post-larvae, Semibalanus balanoides and Elminius modestus, at two temperatures (14 and 19掳C) and two CO2 concentrations (380 and 1,000 ppm), fed with a mixed diatom-flagellate diet at 15,000 cells ml-1 with flow rate of 10 ml-1 min-1. Control growth rates, using operculum diameter, were 14 卤 8 碌m day-1 and 6 卤 2 碌m day-1 for S. balanoides and E. modestus, respectively. Subtle, but significant decreases in E. modestus growth rate were observed in high CO2 but there were no impacts on shell calcium content and survival by either elevated temperature or CO2. S. balanoides exhibited no clear alterations in growth rate but did show a large reduction in shell calcium content and survival under elevated temperature and CO2. These results suggest that a decrease by 0.4 pH(NBS) units alone would not be sufficient to directly impact the survival of barnacles during the first month post-settlement. However, in conjunction with a 4-5掳C increase in temperature, it appears that significant changes to the biology of these organisms will ensue.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="113721032"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="113721032"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 113721032; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=113721032]").text(description); $(".js-view-count[data-work-id=113721032]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 113721032; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='113721032']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 113721032, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=113721032]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":113721032,"title":"Seawater carbonate chemistry and biological processes during experiments with postlarvae of barnacle of Semibalanus balanoides and Elminius modestus, 2010","translated_title":"","metadata":{"abstract":"Ocean acidification and global warming are occurring concomitantly, yet few studies have investigated how organisms will respond to increases in both temperature and CO2. 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These results suggest that a decrease by 0.4 pH(NBS) units alone would not be sufficient to directly impact the survival of barnacles during the first month post-settlement. However, in conjunction with a 4-5掳C increase in temperature, it appears that significant changes to the biology of these organisms will ensue.","publication_date":{"day":29,"month":3,"year":2010,"errors":{}}},"translated_abstract":"Ocean acidification and global warming are occurring concomitantly, yet few studies have investigated how organisms will respond to increases in both temperature and CO2. Intertidal microcosms were used to examine growth, shell mineralogy and survival of two intertidal barnacle post-larvae, Semibalanus balanoides and Elminius modestus, at two temperatures (14 and 19掳C) and two CO2 concentrations (380 and 1,000 ppm), fed with a mixed diatom-flagellate diet at 15,000 cells ml-1 with flow rate of 10 ml-1 min-1. 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Comeau, S, Gorsky, G, Jeffree, R, Teyssle, JL and Gattuso, JP. 2009. Impact of ocean ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">... 200912. Comeau, S, Gorsky, G, Jeffree, R, Teyssle, JL and Gattuso, JP. 2009. Impact of ocean acidification on a key Arctic pelagic mollusc (Limacina helicina). Biogeosciences , 6: 1877聳82. ... 200912. 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Increasing atmospheric CO2 is causing increasing warming and ice melting as well as a concomitant change in ocean chemistry (&quot;ocean acidification&quot;). As temperature increases it is expected that many temperate species will expand their geographic distribution northwards to follow this thermal shift; however with the addition of ocean acidification this transition may not be so straightforward. Here we investigate the potential impacts of ocean acidification and climate change on populations of an intertidal species, in this case the barnacle Semibalanus balanoides, at the northern edge of its range. Growth and development of metamorphosing post-larvae were negatively impacted at lower pH (pH 7.7) compared to the control (pH 8.1) but were not affected by elevated temperature (+4 掳C). The mineral composition of the shells did not alter under any of the treatments. 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window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=62438260]").text(description); $(".js-view-count[data-work-id=62438260]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 62438260; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='62438260']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 62438260, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "2cae0543d2d0ec0522926c875d47b655" } } $('.js-work-strip[data-work-id=62438260]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":62438260,"title":"Calcification, a physiological process to be considered in the context of the whole organism","translated_title":"","metadata":{"publisher":"Copernicus GmbH","grobid_abstract":"Marine organisms that produce calcium carbonate structures are predicted to be most vulnerable to a decline in oceanic pH (ocean acidification) based on the understanding that calcification rates will decrease as a result of changes in the seawater carbonate chemistry thereby reducing carbonate ion concentration (and associated saturation states). Coastal seas are critical components of the global carbon cycle yet little research has been conducted on acidification impacts on coastal benthic organisms. Here, a critical appraisal of calcification in six benthic species showed, contrary to popular predictions, calcification can increase, and not decrease, in acidified seawater. Measuring the changes in calcium in isolated calcium carbonate structure as well as structures from live animals exposed to acidified seawater allowed a comparison between a species' ability to calcify and the dissolution affects across decreasing levels of pH. Calcium carbonate production is dependant on the ability to increase calcification thus counteracting an increase in dissolution. Comparison with paleoecological studies of past high carbon dioxide (CO 2) events presents a similar picture. This conclusion implies that calcification may not be the critical process impacted by ocean acidification; particularly as all species investigated displayed physiological trade offs including reduced metabolism, health, and behavioural responses, in association with this calcification upregulation, which possess as great a threat to survival as an inability to calcify.","publication_name":"Biogeosciences Discussions","grobid_abstract_attachment_id":75203021},"translated_abstract":null,"internal_url":"https://www.academia.edu/62438260/Calcification_a_physiological_process_to_be_considered_in_the_context_of_the_whole_organism","translated_internal_url":"","created_at":"2021-11-26T01:28:28.118-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":90363891,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":75203021,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/75203021/thumbnails/1.jpg","file_name":"Calcification_a_physiological_process_to20211126-28945-1frveaq.pdf","download_url":"https://www.academia.edu/attachments/75203021/download_file?st=MTczMjk4MTIwOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Calcification_a_physiological_process_to.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/75203021/Calcification_a_physiological_process_to20211126-28945-1frveaq.pdf?1637918976=\u0026response-content-disposition=attachment%3B+filename%3DCalcification_a_physiological_process_to.pdf\u0026Expires=1732978495\u0026Signature=Zt2FusJ1nEKjfAPHivROoHotAQE-z-IR47RHv5YyxbE~V0dAsJNpDyskszrIJtrM3GOjpX0yGy~r8TV-Bt-JAvCwbA6N2BOa0DqlNS~zga4ID0vUPQA-~gqBBooA9gk7oaYm0sEwRy6J4hRv2Z4sLcve6zWOsIPY7xhfyGWvInvIU3vYqTGNXUdbvJYfH67POJTLnOhfkly3QwfBweIY7zCO6hEmDPyKsrtchaQj4DtQzeM1HWmI4OSl3a8sYx~nmDZ6P2euI5~KdLPtctIFRvYJ4zTivz~7RSZf6Ur0pKAE8rXMNlGDTu~Iyk~x6DtT1hTA46MV86tvkIKuKCNQUw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Calcification_a_physiological_process_to_be_considered_in_the_context_of_the_whole_organism","translated_slug":"","page_count":18,"language":"en","content_type":"Work","owner":{"id":90363891,"first_name":"Mike","middle_initials":null,"last_name":"Kendall","page_name":"MikeKendall6","domain_name":"independent","created_at":"2018-09-07T05:51:20.536-07:00","display_name":"Mike Kendall","url":"https://independent.academia.edu/MikeKendall6"},"attachments":[{"id":75203021,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/75203021/thumbnails/1.jpg","file_name":"Calcification_a_physiological_process_to20211126-28945-1frveaq.pdf","download_url":"https://www.academia.edu/attachments/75203021/download_file?st=MTczMjk4MTIwOCw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Calcification_a_physiological_process_to.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/75203021/Calcification_a_physiological_process_to20211126-28945-1frveaq.pdf?1637918976=\u0026response-content-disposition=attachment%3B+filename%3DCalcification_a_physiological_process_to.pdf\u0026Expires=1732978495\u0026Signature=Zt2FusJ1nEKjfAPHivROoHotAQE-z-IR47RHv5YyxbE~V0dAsJNpDyskszrIJtrM3GOjpX0yGy~r8TV-Bt-JAvCwbA6N2BOa0DqlNS~zga4ID0vUPQA-~gqBBooA9gk7oaYm0sEwRy6J4hRv2Z4sLcve6zWOsIPY7xhfyGWvInvIU3vYqTGNXUdbvJYfH67POJTLnOhfkly3QwfBweIY7zCO6hEmDPyKsrtchaQj4DtQzeM1HWmI4OSl3a8sYx~nmDZ6P2euI5~KdLPtctIFRvYJ4zTivz~7RSZf6Ur0pKAE8rXMNlGDTu~Iyk~x6DtT1hTA46MV86tvkIKuKCNQUw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":68527,"name":"Ocean acidification","url":"https://www.academia.edu/Documents/in/Ocean_acidification"},{"id":82100,"name":"Global Carbon Cycle","url":"https://www.academia.edu/Documents/in/Global_Carbon_Cycle"},{"id":151321,"name":"Biogeosciences","url":"https://www.academia.edu/Documents/in/Biogeosciences"}],"urls":[{"id":14504512,"url":"http://www.biogeosciences-discuss.net/6/2267/2009/bgd-6-2267-2009.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="62438259"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/62438259/The_stability_of_the_deposit_feeding_community_of_a_mud_flat_in_the_River_Tees"><img alt="Research paper thumbnail of The stability of the deposit feeding community of a mud flat in the River Tees" class="work-thumbnail" src="https://attachments.academia-assets.com/75203010/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/62438259/The_stability_of_the_deposit_feeding_community_of_a_mud_flat_in_the_River_Tees">The stability of the deposit feeding community of a mud flat in the River Tees</a></div><div class="wp-workCard_item"><span>Estuarine and Coastal Marine Science</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="42a2308aedab587806271b91cba8ea39" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":75203010,"asset_id":62438259,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/75203010/download_file?st=MTczMjk4MTIwOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="62438259"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="62438259"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 62438259; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=62438259]").text(description); $(".js-view-count[data-work-id=62438259]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 62438259; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='62438259']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 62438259, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="62438255"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/62438255/Variations_in_some_morphological_characteristics_of_Polydora_ciliata_Johnston_"><img alt="Research paper thumbnail of Variations in some morphological characteristics of Polydora ciliata (Johnston)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/62438255/Variations_in_some_morphological_characteristics_of_Polydora_ciliata_Johnston_">Variations in some morphological characteristics of Polydora ciliata (Johnston)</a></div><div class="wp-workCard_item"><span>Http Dx Doi Org 10 1080 00222938000770351</span><span>, Feb 17, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT On investigation of a dense population of mud tube building polychaetes tentatively iden...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT On investigation of a dense population of mud tube building polychaetes tentatively identified as Polydora ciliata it was found that many individuals also showed morphological characteristics more usually associated with other members of the same genus. This prompted the examination of the morphology of P. ciliata from a number of different areas with the aim of assessing the stability of some of the characters used in the taxonomy of its genus. These proved to be highly variable, did not group together consistently and overlapped with some of those of P. limicola (Annenkova) and P. ligni Webster. No clear distinction between P. ciliata and P. limicola could be made on the grounds of the characteristics examined but the overlap between P. ciliata and P. ligni was small.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="62438255"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="62438255"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 62438255; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=62438255]").text(description); $(".js-view-count[data-work-id=62438255]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 62438255; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='62438255']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 62438255, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=62438255]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":62438255,"title":"Variations in some morphological characteristics of Polydora ciliata (Johnston)","translated_title":"","metadata":{"abstract":"ABSTRACT On investigation of a dense population of mud tube building polychaetes tentatively identified as Polydora ciliata it was found that many individuals also showed morphological characteristics more usually associated with other members of the same genus. This prompted the examination of the morphology of P. ciliata from a number of different areas with the aim of assessing the stability of some of the characters used in the taxonomy of its genus. These proved to be highly variable, did not group together consistently and overlapped with some of those of P. limicola (Annenkova) and P. ligni Webster. No clear distinction between P. ciliata and P. limicola could be made on the grounds of the characteristics examined but the overlap between P. ciliata and P. ligni was small.","publication_date":{"day":17,"month":2,"year":2007,"errors":{}},"publication_name":"Http Dx Doi Org 10 1080 00222938000770351"},"translated_abstract":"ABSTRACT On investigation of a dense population of mud tube building polychaetes tentatively identified as Polydora ciliata it was found that many individuals also showed morphological characteristics more usually associated with other members of the same genus. This prompted the examination of the morphology of P. ciliata from a number of different areas with the aim of assessing the stability of some of the characters used in the taxonomy of its genus. These proved to be highly variable, did not group together consistently and overlapped with some of those of P. limicola (Annenkova) and P. ligni Webster. No clear distinction between P. ciliata and P. limicola could be made on the grounds of the characteristics examined but the overlap between P. ciliata and P. ligni was small.","internal_url":"https://www.academia.edu/62438255/Variations_in_some_morphological_characteristics_of_Polydora_ciliata_Johnston_","translated_internal_url":"","created_at":"2021-11-26T01:28:27.488-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":90363891,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Variations_in_some_morphological_characteristics_of_Polydora_ciliata_Johnston_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":90363891,"first_name":"Mike","middle_initials":null,"last_name":"Kendall","page_name":"MikeKendall6","domain_name":"independent","created_at":"2018-09-07T05:51:20.536-07:00","display_name":"Mike Kendall","url":"https://independent.academia.edu/MikeKendall6"},"attachments":[],"research_interests":[{"id":155,"name":"Evolutionary Biology","url":"https://www.academia.edu/Documents/in/Evolutionary_Biology"},{"id":173,"name":"Zoology","url":"https://www.academia.edu/Documents/in/Zoology"},{"id":9588,"name":"Natural History","url":"https://www.academia.edu/Documents/in/Natural_History"}],"urls":[{"id":14504508,"url":"http://www.tandfonline.com/doi/abs/10.1080/00222938000770351?journalCode=tnah20"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="62438254"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/62438254/Can_ocean_acidification_affect_population_dynamics_of_the_barnacle_Semibalanus_balanoides_at_its_southern_range_edge"><img alt="Research paper thumbnail of Can ocean acidification affect population dynamics of the barnacle Semibalanus balanoides at its southern range edge?" class="work-thumbnail" src="https://attachments.academia-assets.com/75203016/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/62438254/Can_ocean_acidification_affect_population_dynamics_of_the_barnacle_Semibalanus_balanoides_at_its_southern_range_edge">Can ocean acidification affect population dynamics of the barnacle Semibalanus balanoides at its southern range edge?</a></div><div class="wp-workCard_item"><span>Http Dx Doi Org 10 1890 09 1987 1</span><span>, Oct 1, 2010</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="a7efa224c2cd082e82d5aa994a342923" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":75203016,"asset_id":62438254,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/75203016/download_file?st=MTczMjk4MTIwOCw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="62438254"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="62438254"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 62438254; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=62438254]").text(description); $(".js-view-count[data-work-id=62438254]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 62438254; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='62438254']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 62438254, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "a7efa224c2cd082e82d5aa994a342923" } } $('.js-work-strip[data-work-id=62438254]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":62438254,"title":"Can ocean acidification affect population dynamics of the barnacle Semibalanus balanoides at its southern range edge?","translated_title":"","metadata":{"grobid_abstract":"The global ocean and atmosphere are warming. There is increasing evidence suggesting that, in addition to other environmental factors, climate change is affecting species distributions and local population dynamics. Additionally, as a consequence of the growing levels of atmospheric carbon dioxide (CO 2), the oceans are taking up increasing amounts of this CO 2 , causing ocean pH to decrease (ocean acidification). The relative impacts of ocean acidification on population dynamics have yet to be investigated, despite many studies indicating that there will be at least a sublethal impact on many marine organisms, particularly key calcifying organisms. Using empirical data, we forced a barnacle (Semibalanus balanoides) population model to investigate the relative influence of sea surface temperature (SST) and ocean acidification on a population nearing the southern limit of its geographic distribution. Hindcast models were compared to observational data from Cellar Beach (southwestern United Kingdom). Results indicate that a declining pH trend (脌0.0017 unit/yr), indicative of ocean acidification over the past 50 years, does not cause an observable impact on the population abundance relative to changes caused by fluctuations in temperature. Below the critical temperature (here T crit 录 13.18C), pH has a more significant affect on population dynamics at this southern range edge. However, above this value, SST has the overriding influence. At lower SST, a decrease in pH (according to the National Bureau of Standards, pH NBS) from 8.2 to 7.8 can significantly decrease the population abundance. The lethal impacts of ocean acidification observed in experiments on early life stages reduce cumulative survival by ;25%, which again will significantly alter the population level at this southern limit. 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href="https://www.academia.edu/62438253/Effects_of_bottom_trawling_on_ecosystem_functioning"><img alt="Research paper thumbnail of Effects of bottom trawling on ecosystem functioning" class="work-thumbnail" src="https://attachments.academia-assets.com/75203381/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/62438253/Effects_of_bottom_trawling_on_ecosystem_functioning">Effects of bottom trawling on ecosystem functioning</a></div><div class="wp-workCard_item"><span>Journal of Experimental Marine Biology and Ecology</span><span>, Nov 1, 2008</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="407ecfa75b61ff67d1d161cc7c5c4b35" class="wp-workCard--action" rel="nofollow" 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observations with data from controlled mesocosm experiments this study demonstrated that bottom trawling has the potential to cause long-term impacts on sediment nutrient fluxes. Field observations confirmed that trawling reduced the density of important bioturbators in the study area, but revealed only weak effects of trawling on nutrient fluxes. The importance of the decline in bioturbators was demonstrated in the mesocosm experiments where the density of four key bioturbators (Brissopsis lyrifera, Nuculana minuta, Calocaris macandreae and Amphiura chiajei) showed significant correlations with nutrient flux. All four species caused an increase in the rate at which silicate was released from the sediment, but their effect on nitrogen cycling were species specific. Bioturbators that bulldoze through the sediment (B. lyrifera and N. minuta) increased the loss of dissolved inorganic nitrogen (DIN) from the sediment, whereas those that irrigate burrows within the sediment (C. macandreae and A. chiajei) caused increased uptake of DIN. This shows that the activities of the species present can determine whether the seabed acts as a source or a sink of nitrogen nutrients. By combining these experimental results with field observations of bioturbator abundances, we demonstrate the potential impacts of trawling on benthic ecosystem function. 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