Articles | Volume 18, issue 8
https://doi.org/10.5194/cp-18-1915-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-18-1915-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
24 Aug 2022
Research article |
| 24 Aug 2022
| 24 Aug 2022
A 300 000-year record of cold-water coral mound build-up at the East Melilla Coral Province (SE Alboran Sea, western Mediterranean)
Robin Fentimen
CORRESPONDING AUTHOR
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
present address: Réserves Naturelles de France – Antenne Littorale,
Terre Plein de l'Ecluse, 50400, Granville, France
Eline Feenstra
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
Andres Rüggeberg
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
Efraim Hall
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
Valentin Rime
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
Torsten Vennemann
Institute of Earth Surface Dynamics, University of Lausanne,
Lausanne, 1015, Switzerland
Irka Hajdas
Laboratory of Ion Beam Physics, ETH Zürich, Zürich, 8093,
Switzerland
Antonietta Rosso
Department of Biological, Geological and Environmental Sciences,
University of Catania, Catania, 95128, Italy
David Van Rooij
Department of Geology, Ghent University, Ghent, 9000, Belgium
Thierry Adatte
Institute of Earth Surface Dynamics, University of Lausanne,
Lausanne, 1015, Switzerland
Hendrik Vogel
Institute of Geological Sciences and Oeschger Centre for Climate
Change Research, University of Bern, Bern, 3012, Switzerland
Norbert Frank
Institute of Environmental Physics, University of Heidelberg,
69120 Heidelberg, Germany
Anneleen Foubert
Department of Geosciences, University of Fribourg, Fribourg, 1700,
Switzerland
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Giuseppe Maruca, Mara Cipriani, Rocco Dominici, Gianpietro Imbrogno, Giovanni Vespasiano, Carmine Apollaro, Francesco Perri, Fabio Bruno, Antonio Lagudi, Umberto Severino, Valentina A. Bracchi, Daniela Basso, Emilio Cellini, Fabrizio Mauri, Antonietta Rosso, Rossana Sanfilippo, and Adriano Guido
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The Dallol area (northern Afar, Ethiopia) is the ideal field lab to study the birth of a future ocean. The ADD-ON workshop brought together scientists from different disciplines, government agencies, local universities, and communities to plan a scientific drilling into the Dallol deep subsurface. This drilling will provide unique archives to resolve questions related to rift processes, seismic and volcanic activity, climate change, the deep biosphere, geothermal energy, and water resources.
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We found that novel ecosystems created by glacier retreat are first characterized by an increase in plant diversity that is driven by a shift in soil texture. Plant diversity in turn increases soil organic matter and nutrient. Soils gradually acidifies and leads to a final stage where a dominance of few plant species reduces plant diversity. Understanding plant–soil interactions is crucial to anticipate how glacier retreat shapes biodiversity and landscapes.
Marcel Ortler, Achim Brauer, Stefano C. Fabbri, Jean Nicolas Haas, Irka Hajdas, Kerstin Kowarik, Jochem Kueck, Hans Reschreiter, and Michael Strasser
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The lake drilling project at Lake Hallstatt (Austria) successfully cored 51 m of lake sediments. This was achieved through the novel drilling platform Hipercorig. A core-log seismic correlation was created for the first time of an inner Alpine lake of the Eastern Alps. The sediments cover over 12 000 years before present with 10 (up to 5.1 m thick) instantaneous deposits. Lake Hallstatt is located within an UNESCO World Heritage area which has a rich history of human salt mining.
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Moussa Moustapha, Loris Deirmendjian, David Sebag, Jean-Jacques Braun, Stéphane Audry, Henriette Ateba Bessa, Thierry Adatte, Carole Causserand, Ibrahima Adamou, Benjamin Ngounou Ngatcha, and Frédéric Guérin
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Biochemical reactions related to hydrocarbon seepage are known to induce carbonates in marine sediments. Seep carbonates may act as seals and force lateral deviations of rising hydrocarbons. However, crustacean burrows may act as efficient vertical fluid channels allowing hydrocarbons to pass through upward, thereby allowing the vertical growth of carbonate stacks over time. This mechanism may explain the origin of carbonate columns in marine sediments throughout hydrocarbon provinces worldwide.
Stamatina Makri, Andrea Lami, Luyao Tu, Wojciech Tylmann, Hendrik Vogel, and Martin Grosjean
Biogeosciences, 18, 1839–1856, https://doi.org/10.5194/bg-18-1839-2021, https://doi.org/10.5194/bg-18-1839-2021, 2021
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Anoxia in lakes is a major growing concern. In this study we applied a multiproxy approach combining high-resolution hyperspectral imaging (HSI) pigment data with specific HPLC data to examine the Holocene evolution and main drivers of lake anoxia and trophic state changes. We find that when human impact was low, these changes were driven by climate and natural lake-catchment evolution. In the last 500 years, increasing human impact has promoted lake eutrophication and permanent anoxia.
Louis Honegger, Thierry Adatte, Jorge E. Spangenberg, Miquel Poyatos-Moré, Alexandre Ortiz, Magdalena Curry, Damien Huyghe, Cai Puigdefàbregas, Miguel Garcés, Andreu Vinyoles, Luis Valero, Charlotte Läuchli, Andrés Nowak, Andrea Fildani, Julian D. Clark, and Sébastien Castelltort
Solid Earth Discuss., https://doi.org/10.5194/se-2021-12, https://doi.org/10.5194/se-2021-12, 2021
Publication in SE not foreseen
Lydia R. Bailey, Filippo L. Schenker, Maria Giuditta Fellin, Miriam Cobianchi, Thierry Adatte, and Vincenzo Picotti
Solid Earth, 11, 2463–2485, https://doi.org/10.5194/se-11-2463-2020, https://doi.org/10.5194/se-11-2463-2020, 2020
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The Kallipetra Basin, formed in the Late Cretaceous on the reworked Pelagonian–Axios–Vardar contact in the Hellenides, is described for the first time. We document how and when the basin evolved in response to tectonic forcings and basin inversion. Cenomanian extension and basin widening was followed by Turonian compression and basin inversion. Thrusting occurred earlier than previously reported in the literature, with a vergence to the NE, at odds with the regional SW vergence of the margin.
Zhisheng An, Peizhen Zhang, Hendrik Vogel, Yougui Song, John Dodson, Thomas Wiersberg, Xijie Feng, Huayu Lu, Li Ai, and Youbin Sun
Sci. Dril., 28, 63–73, https://doi.org/10.5194/sd-28-63-2020, https://doi.org/10.5194/sd-28-63-2020, 2020
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Earth has experienced remarkable climate–environmental changes in the last 65 million years. The Weihe Basin with its 6000–8000 m infill of a continuous sedimentary sequence gives a unique continental archive for the study of the Cenozoic environment and exploration of deep biospheres. This workshop report concludes key objectives of the two-phase Weihe Basin Drilling Project and the global significance of reconstructing Cenozoic climate evolution and tectonic–monsoon interaction in East Asia.
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Short summary
The investigation of a 9 m long sediment core recovered at ca. 300 m water depth demonstrates that cold-water coral mound build-up within the East Melilla Coral Province (southeastern Alboran Sea) took place during both interglacial and glacial periods. Based on the combination of different analytical methods (e.g. radiometric dating, micropaleontology), we propose that corals never thrived but rather developed under stressful environmental conditions.
The investigation of a 9 m long sediment core recovered at ca. 300 m water depth demonstrates...
