Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco - Research Explorer The University of Manchester

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page-section-publications page-section-publications-view "> <section class="page-section-header page-section-header-publications page-section-header-publications-view no-backdrop-image" data-stickyheader="" style=""> <div class="container"> <div class="row"> <div class="introduction no-metrics"> <div class="rendering"><h1><span>Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco</span></h1></div> <div class="rendering rendering_researchoutput rendering_researchoutput_associatespersonsclassifiedportal rendering_contributiontojournal rendering_associatespersonsclassifiedportal rendering_contributiontojournal_associatespersonsclassifiedportal"><p class="relations persons">Aude Marie Luce Fran Duval-Arnould, Luc Georges Bulot, Rémi Charton, Sreepat Jain, Moussa Masrour, Luis Pomar, <a rel="Person" href="https://research.manchester.ac.uk/en/persons/jonathan.redfern" class="link person"><span>Jonathan Redfern</span></a>, Mike Simmons, <a rel="Person" href="https://research.manchester.ac.uk/en/persons/stefan.schroeder" class="link person"><span>Stefan Schröder</span></a></div> <div class="rendering rendering_researchoutput rendering_researchoutput_associatesorganisationsportal rendering_contributiontojournal rendering_associatesorganisationsportal rendering_contributiontojournal_associatesorganisationsportal"><ul class="relations organisations"><li class="5"><a rel="Organisation" href="https://research.manchester.ac.uk/en/organisations/earth-and-environmental-sciences-academic-research" class="link"><span>Earth and Environmental Sciences - Academic & Research</span></a></li></ul></div> <div class="rendering rendering_researchoutput rendering_researchoutput_associatesexternalorganisationsportal rendering_contributiontojournal rendering_associatesexternalorganisationsportal rendering_contributiontojournal_associatesexternalorganisationsportal"><ul class="relations organisations"><li><a rel="UEOExternalOrganisation" href="#" class="link"><span>Technische Universiteit Delft</span></a></li><li><a rel="UEOExternalOrganisation" href="#" class="link"><span>Adama Science and Technology University</span></a></li><li><a rel="UEOExternalOrganisation" href="#" class="link"><span>Laboratoire de Géologie Appliquée et Géo-Environnement (LAGAGE)</span></a></li><li><a rel="UEOExternalOrganisation" href="#" class="link"><span>Universitat de les Illes Balears (E PALMA01)</span></a></li><li><a rel="UEOExternalOrganisation" href="#" class="link"><span>Neftex-Halliburton</span></a></li></ul></div> <div class="rendering rendering_researchoutput rendering_researchoutput_publicationcontenttyperendererportalng rendering_contributiontojournal rendering_publicationcontenttyperendererportalng rendering_contributiontojournal_publicationcontenttyperendererportalng"><p class="type"><span class="type_family">Research output<span class="type_family_sep">: </span></span><span class="type_classification_parent">Contribution to journal<span class="type_parent_sep"> › </span></span><span class="type_classification">Article</span><span class="type_classification"><span class="type_parent_sep"> › </span>peer-review</span></p></div> </div> <div class="publication-metrics" aria-label="Publication metrics section"> <div class="metrics-container"> <div class="metrics-wrap metrics-bottom "> <div class="metric metric-plum-x"> <a href="https://plu.mx/plum/a/?doi=10.1016/j.jafrearsci.2024.105206" class="plumx-plum-print-popup" data-on-empty="plumXError" data-on-fail="plumXError" data-on-success="plumXSuccess" data-popup="left" data-hide-when-empty="true" data-site="plum" data-badge="false"></a> </div> <div class="metric metric-altmetric"> <div data-badge-popover="top" data-badge-type="donut" data-doi="10.1016/j.jafrearsci.2024.105206" data-hide-no-mentions="true" data-link-target='_blank' class="altmetric-embed"></div> </div> </div> </div> </div> </div> </div> <div class="subMenu"> <div class="content-profile-navigation"> <div class="container"> <nav role="navigation"> <ul class="has-overflow-navigation" role="menubar"> <li class="selected" role="none"> <a class="portal_link" role="menuitem" href="/en/publications/architecture-of-oxfordian-coral-buildups-along-the-atlantic-margi"><span> <i class="icon icon-publication" aria-hidden="true"></i> <span class="label">Overview</span> </span></a> </li> <li class="" role="none"> <a class="portal_link" role="menuitem" href="/en/publications/architecture-of-oxfordian-coral-buildups-along-the-atlantic-margi/fingerprints/"><span> <i class="icon icon-fingerprint" aria-hidden="true"></i> <span class="label">Fingerprint</span> </span></a> </li> </ul> </nav> </div> </div> </div> </section> <div id="main-content" class="page-section-content page-section-content-publications page-section-content-publications-view no-margin "> <section class="page-section content-relation-section"> <div class="container"> <div class="clearfix"> <div class="content-content publication-content"> <h2 class="subheader">Abstract</h2> <div class="rendering rendering_researchoutput rendering_researchoutput_abstractportal rendering_contributiontojournal rendering_abstractportal rendering_contributiontojournal_abstractportal"><div class="textblock">Oxfordian (Upper Jurassic) coral buildups developed widely in Tethys and Atlantic realms, during a time when paleoclimate potentially swung between greenhouse climate and cold snaps. Buildups were constructed by platy and branching corals, sponges and microbialites. Although their initiation is commonly linked to the Upper Jurassic global transgression, a number of global and local factors may have influenced buildup growth and demise (e.g. climate, shelf geometry, detrital input). Extensive outcrops of Oxfordian buildups in Morocco provide an opportunity to investigate the relationship between external drivers and buildup fauna and architecture. Here we show that the interplay of local accommodation changes, rising sea water temperature, and increasing pCO2 linked to the onset of the Middle Oxfordian global transgression were the main drivers for buildup initiation, which was synchronous across the basin. The demise of the coral buildups in Morocco was linked to a regression, dated no later than Upper Oxfordian, the establishment of partly evaporitic conditions across the basin, and to localized influx of coarse-grained siliciclastics, the latter likely driven by synsedimentary tectonic activity. Serial logged sections, outcrop panoramas and detailed facies analysis show that low-relief deeper-water buildups of Dimorpharaea platy corals evolved into higher-relief diversified buildups where shallower-water reworking produced coral rubble and large clinoforms. Buildup diachronicity is apparent, with younger coral bioherms growing in the depressions created between the initial bioherms. Size of buildups ranges from 2 m wide and 0.5 m thick, to 700 m wide and 80 m thick. The outcrops provide constraints on geobody architecture and heterogeneity in the subsurface of Morocco and North America, where facies-controlled dolomitization of high-energy buildup and clinoform facies is a main driver for porosity development.</div></div> <div class="rendering rendering_researchoutput rendering_researchoutput_detailsportal rendering_contributiontojournal rendering_detailsportal rendering_contributiontojournal_detailsportal"><div class="article"><table class="properties"><tbody><tr class="language"><th scope="row">Original language</th><td>English</td></tr><tr><th scope="row">Article number</th><td>105206</td></tr><tr><th scope="row">Journal</th><td><a rel="Journal" href="#" class="link"><span>Journal of African Earth Sciences</span></a></td></tr><tr><th scope="row">Volume</th><td>213</td></tr><tr><th scope="row">Early online date</th><td><span class="date">26 Mar 2024</span></td></tr><tr class="digital_object_identifiers"><th scope="row">DOIs</th><td><ul class="relations digital_object_identifiers"><li><a onclick="window.open(this.href, '_blank','noopener,noreferrer'); return false;" href="https://doi.org/10.1016/j.jafrearsci.2024.105206" class="link"><span>https://doi.org/10.1016/j.jafrearsci.2024.105206</span></a> </li></ul></td></tr><tr class="status"><th scope="row">Publication status</th><td><span class="prefix">Published - </span><span class="date">May 2024</span></td></tr></tbody></table></div></div> <div class="rendering rendering_keywordable rendering_expertkeywordgrouspbytypeportal rendering_keywordable_expertkeywordgrouspbytypeportal"><div class="keyword-group"><h2 class="subheader">Keywords</h2><ul class="relations keywords"><li class="userdefined-keyword"><span>Coral buildup</span></li><li class="userdefined-keyword"><span>Oxfordian</span></li><li class="userdefined-keyword"><span>Platy coral</span></li><li class="userdefined-keyword"><span>Reef architecture</span></li><li class="userdefined-keyword"><span>Subsurface analog</span></li></ul></div></div> </div> <div class="content-sidebar publication-sidebar"> <h2 class="subheader">Access to Document</h2> <div class="rendering rendering_researchoutput rendering_researchoutput_publicationaccessrenderer rendering_contributiontojournal rendering_publicationaccessrenderer rendering_contributiontojournal_publicationaccessrenderer"><ul class="dois"><li class="open-access"><div class="doi"><a onclick="window.open(this.href, '_blank','noopener,noreferrer'); return false;" href="https://doi.org/10.1016/j.jafrearsci.2024.105206" class="link"><span>10.1016/j.jafrearsci.2024.105206</span></a><span class="meta">Licence: <a onclick="window.open(this.href, '_blank','noopener,noreferrer'); return false;" href="http://creativecommons.org/licenses/by/4.0/" class="link">CC BY</a></span></div></li></ul></div> <h2 class="subheader">Other files and links</h2> <div class="rendering rendering_researchoutput rendering_researchoutput_publicationotherfilesandlinksrenderer rendering_contributiontojournal rendering_publicationotherfilesandlinksrenderer rendering_contributiontojournal_publicationotherfilesandlinksrenderer"><ul class="links"><li><div class="link"><a onclick="window.open(this.href, '_blank','noopener,noreferrer'); return false;" href="http://www.scopus.com/inward/record.url?scp=85188833400&partnerID=8YFLogxK" class="link"><span>Link to publication in Scopus</span></a></div></li><li><div class="link"><a onclick="window.open(this.href, '_blank','noopener,noreferrer'); return false;" href="https://www.mendeley.com/catalogue/08522def-6287-34c9-8fd7-443019530370/" class="link"><span>https://www.mendeley.com/catalogue/08522def-6287-34c9-8fd7-443019530370/</span></a></div></li></ul></div> </div> </div> </div> </section> <section class="page-section content-relation-section publication-fingerprint"> <div class="container"> <div class="header"> <h2 class="section-title"> <i class="icon icon-fingerprint" aria-hidden="true"></i> <span class="title">Fingerprint</span> </h2> <span class="sub-title"> Dive into the research topics of 'Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco'. 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M. L. F., Bulot, L. G., Charton, R., Jain, S., Masrour, M., Pomar, L.<a rel="Person" href="https://research.manchester.ac.uk/en/persons/jonathan.redfern" class="link"><span>, Redfern, J.</span></a>, Simmons, M.<a rel="Person" href="https://research.manchester.ac.uk/en/persons/stefan.schroeder" class="link"><span>, & Schröder, S.</span></a> (2024). <a rel="ContributionToJournal" href="https://research.manchester.ac.uk/en/publications/architecture-of-oxfordian-coral-buildups-along-the-atlantic-margi" class="link"><span>Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco</span></a>. <a rel="Journal" href="#" class="link"><span><em>Journal of African Earth Sciences</em></span></a>, <em>213</em>, Article 105206. <a onclick="window.open(this.href, '_blank','noopener,noreferrer'); return false;" href="https://doi.org/10.1016/j.jafrearsci.2024.105206" class="link"><span>https://doi.org/10.1016/j.jafrearsci.2024.105206</span></a></div> </div> <div id="cite-author" class="tab " role="tabpanel" aria-labelledby="tab-1" tabindex="-1" aria-hidden="true"> <div class="rendering rendering_researchoutput rendering_researchoutput_author rendering_contributiontojournal rendering_author rendering_contributiontojournal_author">Duval-Arnould, Aude Marie Luce Fran ; Bulot, Luc Georges ; Charton, Rémi et al. / <a rel="ContributionToJournal" href="https://research.manchester.ac.uk/en/publications/architecture-of-oxfordian-coral-buildups-along-the-atlantic-margi" class="link"><span><strong>Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco</strong></span></a>. In: <a rel="Journal" href="#" class="link"><span>Journal of African Earth Sciences</span></a>. 2024 ; Vol. 213.</div> </div> <div id="cite-BIBTEX" class="tab " role="tabpanel" aria-labelledby="tab-2" tabindex="-1" aria-hidden="true"> <div class="rendering rendering_researchoutput rendering_researchoutput_bibtex rendering_contributiontojournal rendering_bibtex rendering_contributiontojournal_bibtex"><div>@article{cc412d63a9514f61af236c7889388c7e,</div><div> title = "Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco",</div><div> abstract = "Oxfordian (Upper Jurassic) coral buildups developed widely in Tethys and Atlantic realms, during a time when paleoclimate potentially swung between greenhouse climate and cold snaps. Buildups were constructed by platy and branching corals, sponges and microbialites. Although their initiation is commonly linked to the Upper Jurassic global transgression, a number of global and local factors may have influenced buildup growth and demise (e.g. climate, shelf geometry, detrital input). Extensive outcrops of Oxfordian buildups in Morocco provide an opportunity to investigate the relationship between external drivers and buildup fauna and architecture. Here we show that the interplay of local accommodation changes, rising sea water temperature, and increasing pCO2 linked to the onset of the Middle Oxfordian global transgression were the main drivers for buildup initiation, which was synchronous across the basin. The demise of the coral buildups in Morocco was linked to a regression, dated no later than Upper Oxfordian, the establishment of partly evaporitic conditions across the basin, and to localized influx of coarse-grained siliciclastics, the latter likely driven by synsedimentary tectonic activity. Serial logged sections, outcrop panoramas and detailed facies analysis show that low-relief deeper-water buildups of Dimorpharaea platy corals evolved into higher-relief diversified buildups where shallower-water reworking produced coral rubble and large clinoforms. Buildup diachronicity is apparent, with younger coral bioherms growing in the depressions created between the initial bioherms. Size of buildups ranges from 2 m wide and 0.5 m thick, to 700 m wide and 80 m thick. The outcrops provide constraints on geobody architecture and heterogeneity in the subsurface of Morocco and North America, where facies-controlled dolomitization of high-energy buildup and clinoform facies is a main driver for porosity development.",</div><div> keywords = "Coral buildup, Oxfordian, Platy coral, Reef architecture, Subsurface analog",</div><div> author = "Duval-Arnould, {Aude Marie Luce Fran} and Bulot, {Luc Georges} and R{\'e}mi Charton and Sreepat Jain and Moussa Masrour and Luis Pomar and Jonathan Redfern and Mike Simmons and Stefan Schr{\"o}der",</div><div> year = "2024",</div><div> month = may,</div><div> doi = "10.1016/j.jafrearsci.2024.105206",</div><div> language = "English",</div><div> volume = "213",</div><div> journal = "Journal of African Earth Sciences",</div><div> issn = "1464-343X",</div><div> publisher = "Elsevier BV",</div><p>}</p></div> </div> <div id="cite-harvard" class="tab " role="tabpanel" aria-labelledby="tab-3" tabindex="-1" aria-hidden="true"> <div class="rendering rendering_researchoutput rendering_researchoutput_harvard rendering_contributiontojournal rendering_harvard rendering_contributiontojournal_harvard">Duval-Arnould, AMLF, Bulot, LG, Charton, R, Jain, S, Masrour, M, Pomar, L<a rel="Person" href="https://research.manchester.ac.uk/en/persons/jonathan.redfern" class="link"><span>, Redfern, J</span></a>, Simmons, M<a rel="Person" href="https://research.manchester.ac.uk/en/persons/stefan.schroeder" class="link"><span> & Schröder, S</span></a> 2024, '<a rel="ContributionToJournal" href="https://research.manchester.ac.uk/en/publications/architecture-of-oxfordian-coral-buildups-along-the-atlantic-margi" class="link harvard_title"><span>Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco</span></a>', <a rel="Journal" href="#" class="link"><span><em>Journal of African Earth Sciences</em></span></a>, vol. 213, 105206. <a onclick="window.open(this.href, '_blank','noopener,noreferrer'); return false;" href="https://doi.org/10.1016/j.jafrearsci.2024.105206" class="link"><span>https://doi.org/10.1016/j.jafrearsci.2024.105206</span></a></div> </div> <div id="cite-standard" class="tab " role="tabpanel" aria-labelledby="tab-4" tabindex="-1" aria-hidden="true"> <div class="rendering rendering_researchoutput rendering_researchoutput_standard rendering_contributiontojournal rendering_standard rendering_contributiontojournal_standard"><a rel="ContributionToJournal" href="https://research.manchester.ac.uk/en/publications/architecture-of-oxfordian-coral-buildups-along-the-atlantic-margi" class="link"><span><strong>Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco.</strong></span></a> / Duval-Arnould, Aude Marie Luce Fran; Bulot, Luc Georges; Charton, Rémi et al. <br />In: <a rel="Journal" href="#" class="link"><span>Journal of African Earth Sciences</span></a>, Vol. 213, 105206, 05.2024.<p class="type"><span class="type_family">Research output<span class="type_family_sep">: </span></span><span class="type_classification_parent">Contribution to journal<span class="type_parent_sep"> › </span></span><span class="type_classification">Article</span><span class="type_classification"><span class="type_parent_sep"> › </span>peer-review</span></p></div> </div> <div id="cite-RIS" class="tab " role="tabpanel" aria-labelledby="tab-5" tabindex="-1" aria-hidden="true"> <div class="rendering rendering_researchoutput rendering_researchoutput_ris rendering_contributiontojournal rendering_ris rendering_contributiontojournal_ris"><p>TY - JOUR</p><p>T1 - Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco</p><p>AU - Duval-Arnould, Aude Marie Luce Fran</p><p>AU - Bulot, Luc Georges</p><p>AU - Charton, Rémi</p><p>AU - Jain, Sreepat</p><p>AU - Masrour, Moussa</p><p>AU - Pomar, Luis</p><p>AU - Redfern, Jonathan</p><p>AU - Simmons, Mike</p><p>AU - Schröder, Stefan</p><p>PY - 2024/5</p><p>Y1 - 2024/5</p><p>N2 - Oxfordian (Upper Jurassic) coral buildups developed widely in Tethys and Atlantic realms, during a time when paleoclimate potentially swung between greenhouse climate and cold snaps. Buildups were constructed by platy and branching corals, sponges and microbialites. Although their initiation is commonly linked to the Upper Jurassic global transgression, a number of global and local factors may have influenced buildup growth and demise (e.g. climate, shelf geometry, detrital input). Extensive outcrops of Oxfordian buildups in Morocco provide an opportunity to investigate the relationship between external drivers and buildup fauna and architecture. Here we show that the interplay of local accommodation changes, rising sea water temperature, and increasing pCO2 linked to the onset of the Middle Oxfordian global transgression were the main drivers for buildup initiation, which was synchronous across the basin. The demise of the coral buildups in Morocco was linked to a regression, dated no later than Upper Oxfordian, the establishment of partly evaporitic conditions across the basin, and to localized influx of coarse-grained siliciclastics, the latter likely driven by synsedimentary tectonic activity. Serial logged sections, outcrop panoramas and detailed facies analysis show that low-relief deeper-water buildups of Dimorpharaea platy corals evolved into higher-relief diversified buildups where shallower-water reworking produced coral rubble and large clinoforms. Buildup diachronicity is apparent, with younger coral bioherms growing in the depressions created between the initial bioherms. Size of buildups ranges from 2 m wide and 0.5 m thick, to 700 m wide and 80 m thick. The outcrops provide constraints on geobody architecture and heterogeneity in the subsurface of Morocco and North America, where facies-controlled dolomitization of high-energy buildup and clinoform facies is a main driver for porosity development.</p><p>AB - Oxfordian (Upper Jurassic) coral buildups developed widely in Tethys and Atlantic realms, during a time when paleoclimate potentially swung between greenhouse climate and cold snaps. Buildups were constructed by platy and branching corals, sponges and microbialites. Although their initiation is commonly linked to the Upper Jurassic global transgression, a number of global and local factors may have influenced buildup growth and demise (e.g. climate, shelf geometry, detrital input). Extensive outcrops of Oxfordian buildups in Morocco provide an opportunity to investigate the relationship between external drivers and buildup fauna and architecture. Here we show that the interplay of local accommodation changes, rising sea water temperature, and increasing pCO2 linked to the onset of the Middle Oxfordian global transgression were the main drivers for buildup initiation, which was synchronous across the basin. The demise of the coral buildups in Morocco was linked to a regression, dated no later than Upper Oxfordian, the establishment of partly evaporitic conditions across the basin, and to localized influx of coarse-grained siliciclastics, the latter likely driven by synsedimentary tectonic activity. Serial logged sections, outcrop panoramas and detailed facies analysis show that low-relief deeper-water buildups of Dimorpharaea platy corals evolved into higher-relief diversified buildups where shallower-water reworking produced coral rubble and large clinoforms. Buildup diachronicity is apparent, with younger coral bioherms growing in the depressions created between the initial bioherms. Size of buildups ranges from 2 m wide and 0.5 m thick, to 700 m wide and 80 m thick. The outcrops provide constraints on geobody architecture and heterogeneity in the subsurface of Morocco and North America, where facies-controlled dolomitization of high-energy buildup and clinoform facies is a main driver for porosity development.</p><p>KW - Coral buildup</p><p>KW - Oxfordian</p><p>KW - Platy coral</p><p>KW - Reef architecture</p><p>KW - Subsurface analog</p><p>UR - http://www.scopus.com/inward/record.url?scp=85188833400&partnerID=8YFLogxK</p><p>UR - https://www.mendeley.com/catalogue/08522def-6287-34c9-8fd7-443019530370/</p><p>U2 - 10.1016/j.jafrearsci.2024.105206</p><p>DO - 10.1016/j.jafrearsci.2024.105206</p><p>M3 - Article</p><p>SN - 1464-343X</p><p>VL - 213</p><p>JO - Journal of African Earth Sciences</p><p>JF - Journal of African Earth Sciences</p><p>M1 - 105206</p><p>ER - </p></div> </div> <div id="cite-vancouver" class="tab " role="tabpanel" aria-labelledby="tab-6" tabindex="-1" aria-hidden="true"> <div class="rendering rendering_researchoutput rendering_researchoutput_vancouver rendering_contributiontojournal rendering_vancouver rendering_contributiontojournal_vancouver">Duval-Arnould AMLF, Bulot LG, Charton R, Jain S, Masrour M, Pomar L et al. <span class="title"><a rel="ContributionToJournal" href="https://research.manchester.ac.uk/en/publications/architecture-of-oxfordian-coral-buildups-along-the-atlantic-margi" class="link"><span>Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco</span></a></span>. <a rel="Journal" href="#" class="link"><span>Journal of African Earth Sciences</span></a>. 2024 May;213:105206. 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Architecture of Oxfordian coral buildups along the Atlantic margin of Morocco - Research Explorer The University of Manchester