EGU - Division on Stratigraphy, Sedimentology and Palaeontology (SSP)

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does not have JavaScript enabled, or does not support it. </div> </noscript> <p> This page features highlight articles from EGU's open access journals <a href="https://www.biogeosciences.net/">Biogeosciences</a>, <a href="https://www.climate-of-the-past.net/">Climate of the Past</a>, <a href="https://www.geochronology.net/">Geochronology</a> and <a href="https://www.solid-earth.net/">Solid Earth</a>. 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btn-group-toggle mb-1" data-toggle="buttons"> <label class="btn btn-sm btn-tag"> <input ic-trigger-on="change" id="year_2011" name="year" type="checkbox" autocomplete="off" value="2011"> 2011 </label> </div> </div> <noscript> <button type="submit" class="btn btn-primary">Search</button> </noscript> </div> <div id="sidebar_results" class="col-12 col-lg-9"> <div id="sidebar_results_count" class="d-sm-flex justify-content-between align-items-end"> <p> <span id="sidebar_indicator" aria-hidden="true"> <i class="d-inline-block d-lg-none fas fa-spinner fa-spin fa-3x" aria-hidden="true"></i> <span class="d-none d-lg-inline-block" aria-hidden="true"> <i class="fas fa-spinner fa-spin mr-1" aria-hidden="true"></i> Searching ... </span> </span> <span id="sidebar_count"> 386 items found </span> </p> <div class="d-none d-lg-block"> <div class="btn-group btn-group-sm" role="group" aria-label="Show number of entries"> <a data-ic-limit="10" role="button" class="btn btn-tag active" aria-pressed="true" href="?limit=10">10</a> <a data-ic-limit="20" role="button" class="btn btn-tag " href="?limit=20">20</a> <a data-ic-limit="50" role="button" class="btn btn-tag " href="?limit=50">50</a> </div> </div> </div> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2025/02/14/e8e14e92-a572-4b49-8634-0ec095b51cb0.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2025/02/14/e8e14e92-a572-4b49-8634-0ec095b51cb0.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2025/02/14/e8e14e92-a572-4b49-8634-0ec095b51cb0.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://bg.copernicus.org/articles/22/791/2025/bg-22-791-2025.html">What controls planktic foraminiferal calcification?</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-22-791-2025">10.5194/bg-22-791-2025</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 17 February 2025</li> </ul> <p>Planktic foraminifers are a plankton whose fossilised shell weight is used to reconstruct past environmental conditions such as seawater CO2. However, there is debate about whether other environmental drivers impact shell weight. Here we use a global data compilation and statistics to analyse what controls their weight. We find that the response varies between species and ocean basin, making it important to use regional calibrations and consider which species should be used to reconstruct CO2.</p> <p class="more-link my-1 text-right "><a class="external"href="https://bg.copernicus.org/articles/22/791/2025/bg-22-791-2025.html" aria-label="Read more about What controls planktic foraminiferal calcification?">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2025/01/28/b03b7ca2-1ccc-40eb-9e61-f2db9d4a9ab0.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2025/01/28/b03b7ca2-1ccc-40eb-9e61-f2db9d4a9ab0.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2025/01/28/b03b7ca2-1ccc-40eb-9e61-f2db9d4a9ab0.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/bg-22-473-2025">Assessment framework to predict sensitivity of marine calcifiers to ocean alkalinity enhancement – identification of biological thresholds and importance of precautionary principle</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-22-473-2025">10.5194/bg-22-473-2025</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 31 January 2025</li> </ul> <p>The environmental impacts of ocean alkalinity enhancement (OAE) are unknown. Our synthesis, based on 68 collected studies with 84 unique species, shows that 35 % of species respond positively, 26 % respond negatively, and 39 % show a neutral response to alkalinity addition. Biological thresholds were found from 50 to 500 µmol kg−1 NaOH addition. A precautionary approach is warranted to avoid potential risks, while current regulatory framework needs improvements to assure safe biological limits.</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/bg-22-473-2025" aria-label="Read more about Assessment framework to predict sensitivity of marine calcifiers to ocean alkalinity enhancement – identification of biological thresholds and importance of precautionary principle">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2025/01/17/3c43fb43-d81b-48b0-8687-09f340cabcb0.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2025/01/17/3c43fb43-d81b-48b0-8687-09f340cabcb0.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2025/01/17/3c43fb43-d81b-48b0-8687-09f340cabcb0.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/bg-22-341-2025">Efficiency metrics for ocean alkalinity enhancements under responsive and prescribed atmospheric pCO2 conditions</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-22-341-2025">10.5194/bg-22-341-2025</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 20 January 2025</li> </ul> <p>Marine CO2 removal (mCDR) is a promising technology for removing legacy emissions from the atmosphere. Its indirect nature makes it difficult to assess experimentally; instead one relies heavily on simulation. Many past papers have treated the atmosphere as non-responsive to the intervention studied. We show that even under these simplified assumptions, the increase in ocean CO2 inventory is equal to the equivalent quantity of direct CO2 removals occurring over time, in a realistic atmosphere.</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/bg-22-341-2025" aria-label="Read more about Efficiency metrics for ocean alkalinity enhancements under responsive and prescribed atmospheric pCO2 conditions">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2025/01/15/47d2c2ae-dd48-4249-be82-1c5bcc81563a.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2025/01/15/47d2c2ae-dd48-4249-be82-1c5bcc81563a.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2025/01/15/47d2c2ae-dd48-4249-be82-1c5bcc81563a.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/bg-22-305-2025">Ensemble estimates of global wetland methane emissions over 2000–2020</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-22-305-2025">10.5194/bg-22-305-2025</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 17 January 2025</li> </ul> <p>This study assesses global methane emissions from wetlands between 2000 and 2020 using multiple models. We found that wetland emissions increased by 6–7 Tg CH4 yr-1 in the 2010s compared to the 2000s. Rising temperatures primarily drove this increase, while changes in precipitation and CO2 levels also played roles. Our findings highlight the importance of wetlands in the global methane budget and the need for continuous monitoring to understand their impact on climate change.</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/bg-22-305-2025" aria-label="Read more about Ensemble estimates of global wetland methane emissions over 2000–2020">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2025/01/09/ed8a4d3b-5a0d-407e-9ba8-7287e66ea428.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2025/01/09/ed8a4d3b-5a0d-407e-9ba8-7287e66ea428.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2025/01/09/ed8a4d3b-5a0d-407e-9ba8-7287e66ea428.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/bg-22-71-2025">Particle fluxes by subtropical pelagic communities under ocean alkalinity enhancement</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-22-71-2025">10.5194/bg-22-71-2025</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 10 January 2025</li> </ul> <p>Ocean alkalinity enhancement (OAE) is a negative emission technology which may alter marine communities and the particle export they drive. Here, impacts of carbonate-based OAE on the flux and attenuation of sinking particles in an oligotrophic plankton community are presented. Whilst biological parameters remained unaffected, abiotic carbonate precipitation occurred. Among counteracting OAE’s efficiency, it influenced mineral ballasting and particle sinking velocities, requiring monitoring.</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/bg-22-71-2025" aria-label="Read more about Particle fluxes by subtropical pelagic communities under ocean alkalinity enhancement">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2024/12/20/8da92e26-040d-4ca4-b175-424ddc30d506.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2024/12/20/8da92e26-040d-4ca4-b175-424ddc30d506.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2024/12/20/8da92e26-040d-4ca4-b175-424ddc30d506.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/cp-20-2719-2024">Surface buoyancy control of millennial-scale variations in the Atlantic meridional ocean circulation</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.climate-of-the-past.net/">Climate of the Past</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/cp-20-2719-2024">10.5194/cp-20-2719-2024</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 23 December 2024</li> </ul> <p>Using an Earth system model that can simulate Dansgaard–Oeschger-like events, we show that conditions under which millennial-scale climate variability occurs are related to the integrated surface buoyancy flux over the northern North Atlantic. This newly defined buoyancy measure explains why millennial-scale climate variability arising from abrupt changes in the Atlantic meridional overturning circulation occurred for mid-glacial conditions but not for interglacial or full glacial conditions.</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/cp-20-2719-2024" aria-label="Read more about Surface buoyancy control of millennial-scale variations in the Atlantic meridional ocean circulation">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2024/11/27/6ff42521-d23f-49ee-8127-452c34540216.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2024/11/27/6ff42521-d23f-49ee-8127-452c34540216.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2024/11/27/6ff42521-d23f-49ee-8127-452c34540216.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/bg-21-5305-2024">Microbial response to deliquescence of nitrate-rich soils in the hyperarid Atacama Desert</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-21-5305-2024">10.5194/bg-21-5305-2024</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 29 November 2024</li> </ul> <p>We studied unique nitrate-rich soils in the hyperarid Atacama Desert that form brines at night under high relative humidity. Despite providing water for microorganisms, these soils exhibit extremely low microbial activity, indicating that the high nitrate levels inhibit microbial life. On the other hand, enriched organic matter indicates their potential preservation. This research helps to understand the limits of life in extreme environments and aids in the search for signs of life on Mars.</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/bg-21-5305-2024" aria-label="Read more about Microbial response to deliquescence of nitrate-rich soils in the hyperarid Atacama Desert">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2024/11/25/40799157-7395-4c02-921e-7e373bf8739c.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2024/11/25/40799157-7395-4c02-921e-7e373bf8739c.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2024/11/25/40799157-7395-4c02-921e-7e373bf8739c.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/bg-21-5233-2024">Microbial strong organic-ligand production is tightly coupled to iron in hydrothermal plumes</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-21-5233-2024">10.5194/bg-21-5233-2024</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 29 November 2024</li> </ul> <p>Hydrothermally derived iron can be transported kilometers away from deep-sea vents, representing a significant flux of vital micronutrients to the ocean. However, the mechanisms that support the stabilization of dissolved iron remain elusive. Using electrochemical, spectrometry, and genomic methods, we demonstrated that strong ligands exert an important control on iron in plumes, and high-affinity iron-binding siderophores were identified in several hydrothermal plume samples for the first time</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/bg-21-5233-2024" aria-label="Read more about Microbial strong organic-ligand production is tightly coupled to iron in hydrothermal plumes">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2024/11/28/1b3833c3-5f18-4d38-8620-9371eb8a1298.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2024/11/28/1b3833c3-5f18-4d38-8620-9371eb8a1298.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2024/11/28/1b3833c3-5f18-4d38-8620-9371eb8a1298.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/bg-21-5321-2024">Representation of the terrestrial carbon cycle in CMIP6</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-21-5321-2024">10.5194/bg-21-5321-2024</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 28 November 2024</li> </ul> <p>This study investigates present-day carbon cycle variables in CMIP5 and CMIP6 simulations. Overall, CMIP6 models perform better but also show many remaining biases. A significant improvement in the simulation of photosynthesis in models with a nitrogen cycle is found, with only small differences between emission- and concentration-based simulations. Thus, we recommend using emission-driven simulations in CMIP7 by default and including the nitrogen cycle in all future carbon cycle models.</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/bg-21-5321-2024" aria-label="Read more about Representation of the terrestrial carbon cycle in CMIP6">Read more</a> </div> </article> <hr> <article class="media"> <img role="presentation" alt="" class="img-fluid img-thumbnail" src="https://www.egu.eu/media/news/highlightarticles/2024/11/25/f11ec537-87d8-486c-861a-5708ff80e760.png.120x120_q90_crop_upscale.png" srcset="https://www.egu.eu/media/news/highlightarticles/2024/11/25/f11ec537-87d8-486c-861a-5708ff80e760.png.120x120_q90_crop_upscale.png 1x, https://www.egu.eu/media/news/highlightarticles/2024/11/25/f11ec537-87d8-486c-861a-5708ff80e760.png.240x240_q90_crop_upscale.png 2x" loading="lazy"> <div class="media-body"> <a class="h4 external" href="https://dx.doi.org/10.5194/bg-21-5079-2024">X-BASE: the first terrestrial carbon and water flux products from an extended data-driven scaling framework, FLUXCOM-X</a> <ul class="list-inline mt-1"> <li class="list-inline-item"><i class="far fa-fw fa-newspaper"></i> <a class="external" href="https://www.biogeosciences.net/">Biogeosciences</a></li> <li class="list-inline-item"><abbr class="initialism" title="Digital object identifier">DOI</abbr> <a class="external" href="https://doi.org/10.5194/bg-21-5079-2024">10.5194/bg-21-5079-2024</a></li> <li class="list-inline-item"><i class="far fa-fw fa-calendar-plus"></i> 25 November 2024</li> </ul> <p>The movement of water, carbon, and energy from the Earth’s surface to the atmosphere, or flux, is an important process to understand because it impacts our lives. Here, we outline a method called FLUXCOM-X to estimate global water and CO2 fluxes based on direct measurements from sites around the world. We go on to demonstrate how these new estimates of net CO2 uptake/loss, gross CO2 uptake, total water evaporation, and transpiration from plants compare to previous and independent estimates.</p> <p class="more-link my-1 text-right "><a class="external"href="https://dx.doi.org/10.5194/bg-21-5079-2024" aria-label="Read more about X-BASE: the first terrestrial carbon and water flux products from an extended data-driven scaling framework, FLUXCOM-X">Read more</a> </div> </article> <hr> <nav class="btn-toolbar btn-toolbar-pagination mt-2" role="presentation" aria-label="Pagination navigation"> <div class="btn-group btn-group-sm mx-auto" role="group"> <a href="?page=1" data-ic-page="1" role="button" class="btn btn-tag active" aria-pressed="true">1</a> <a href="?page=2" data-ic-page="2" role="button" class="btn btn-tag">2</a> <a href="?page=3" data-ic-page="3" role="button" class="btn btn-tag">3</a> <a href="#" disabled type="button" class="btn btn-tag disabled">...</a> <a href="?page=39" data-ic-page="39" role="button" class="btn btn-tag">39</a> <a href="?page=2" data-ic-page="2" role="button" class="btn btn-tag" aria-label="Next"> <i class="fas fa-fw fa-angle-double-right" aria-hidden="true"></i> <span class="sr-only">Next</span> </a> </div> </nav> </div> </div> </form> </div> </main>  <footer class="d-print-none"> <div class="footer"> <div class="container"> <div class="row"> <div class="col-md-6 mb-4 mb-md-0"> <div class="footer-heading"> <h2>About EGU</h2> </div> <p>EGU, the European Geosciences Union, is Europe’s premier geosciences union, dedicated to the pursuit of excellence in the Earth, planetary, and space sciences for the benefit of humanity, worldwide. It was established in September 2002 as a merger of the European Geophysical Society (EGS) and the European Union of Geosciences (EUG), and has headquarters in Munich, Germany.</p> <p class="small"> Header image: <a href="https://imaggeo.egu.eu/view/1613/">Explosion</a> (Credit: Fulvia Favaro, distributed via imaggeo.egu.eu) </p> <div class="footer-heading mt-4"> <h2>Follow us</h2> </div> <ul class="list-inline socialicons"> <li class="list-inline-item"><a title="Follow us on X" aria-label="Follow us on X" href="https://x.com/EuroGeosciences"><i class="rounded-sm fab fa-fw fa-x-twitter"></i></a></li><li class="list-inline-item"><a title="Follow us on Facebook" aria-label="Follow us on Facebook" href="https://www.facebook.com/EuropeanGeosciencesUnion"><i class="rounded-sm fab fa-fw fa-facebook"></i></a></li><li class="list-inline-item"><a title="Find us on LinkedIn" aria-label="Find us on LinkedIn" href="https://www.linkedin.com/company/european-geosciences-union"><i class="rounded-sm fab fa-fw fa-linkedin"></i></a></li><li class="list-inline-item"><a title="Find us on Instagram" aria-label="Find us on Instagram" href="https://www.instagram.com/eurogeosciences/"><i class="rounded-sm fab fa-fw fa-instagram"></i></a></li><li class="list-inline-item"><a title="Find us on YouTube" aria-label="Find us on YouTube" href="https://www.youtube.com/user/EuroGeosciencesUnion"><i class="rounded-sm fab fa-fw fa-youtube"></i></a></li> </ul> </div> <div class="col-md-6 mb-4 mb-md-0"> <div class="row"> <div class="col-md-6 mb-4"> <div class="footer-heading"> <h2>Information for</h2> </div> <ul class="list-unstyled list-footer-links"> <li><a href="/membership/benefits/">Researchers</a></li> <li><a href="/ecs/">Early career scientists</a></li> <li><a href="/news/">Media</a></li> <li><a href="/education/">Educators & children</a></li> </ul> </div> <div class="col-md-6 mb-4"> <div class="footer-heading"> <h2>External links</h2> </div> <ul class="list-unstyled list-footer-links"> <li> <a class="external" href="https://www.egu25.eu">General Assembly 2025</a> <small>Europe's largest geoscience conference</small> </li> <li> <a class="external" href="https://blogs.egu.eu/">EGU blogs</a> <small>Blogs hosted by the EGU</small> </li> <li> <a class="external" href="https://imaggeo.egu.eu/">Imaggeo</a> <small>The geosciences image and video repository</small> </li> </ul> </div> </div> <div class="footer-heading"> <h2>EGU Newsletter</h2> </div> <p class="small">Subscribe to our monthly <a href="/newsletter/">newsletter</a> and stay up to date with the latest EGU news.</p> </div> </div> </div> </div> <div class="links"> <div class="container"> <div class="row"> <div class="col-md-12 text-center text-md-left"> <div class="d-lg-flex"> <ul class="list-inline mr-md-5 mb-2 mb-md-0"> <li class="list-inline-item">© 2025 European Geosciences Union</li> </ul> <ul class="list-inline"> <li class="list-inline-item"><a href="/contact/">Contact</a></li> <li class="list-inline-item">|</li> <li class="list-inline-item"><a href="/imprint/">Imprint</a></li> <li class="list-inline-item">|</li> <li class="list-inline-item"><a href="/privacy-policy/">Privacy policy</a></li> <li class="list-inline-item">|</li> <li class="list-inline-item"><a href="/visual-identity/">Visual identity</a></li> </ul> </div> </div> </div> </div> </div> </footer> <script src="https://www.egu.eu/static/8b1788b6/vendors/jquery/jquery.min.js"></script> <script src="https://www.egu.eu/static/8b1788b6/vendors/bootstrap4/js/bootstrap.bundle.min.js"></script> <script src="https://www.egu.eu/static/8b1788b6/js/core.min.js"></script> <noscript><p><img src="https://pwk.egu.eu/p.pwk?idsite=1&rec=1" style="border:0" alt="" /></p></noscript> </body> </html>

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