Science report
| 
27 May 2020
Science report |
| 27 May 2020
| 27 May 2020
High-resolution late Holocene sedimentary cores record the long history of the city of Cádiz (south-western Spain)
Ferréol Salomon
CORRESPONDING AUTHOR
Laboratoire Image Ville Environnement (UMR 7362), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de
l'Argonne, 67000 Strasbourg, France
Darío Bernal-Casasola
Departamento de Historia, Geografía y Filosofía, Área
de Arqueología, Universidad de Cádiz, Avenida Doctor Gómez Ulla
1, 11003 Cádiz, Spain
José J. Díaz
Departamento de Historia, Geografía y Filosofía, Área
de Arqueología, Universidad de Cádiz, Avenida Doctor Gómez Ulla
1, 11003 Cádiz, Spain
Macarena Lara
Departamento de Historia, Geografía y Filosofía, Área
de Arqueología, Universidad de Cádiz, Avenida Doctor Gómez Ulla
1, 11003 Cádiz, Spain
Salvador Domínguez-Bella
Departamento de Ciencias de la Tierra, UGEA-PHAM, Universidad de
Cádiz, Avda. República Saharahui s/n, Campus Rio San Pedro, Puerto
Real, 11510 Cádiz, Spain
Damien Ertlen
Laboratoire Image Ville Environnement (UMR 7362), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de
l'Argonne, 67000 Strasbourg, France
Patrick Wassmer
Laboratoire Image Ville Environnement (UMR 7362), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de
l'Argonne, 67000 Strasbourg, France
Laboratoire de Géographie Physique (UMR-8591), Centre National de la Recherche Scientifique (CNRS)/ Université Paris 1,
Panthéon-Sorbonne, 1 Place Aristide Briand, 92195 Meudon, France
Pierre Adam
Institut de Chimie de Strasbourg, Biogéochimie moléculaire
(UMR-7177), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 4 rue Blaise Pascal, 67000 Strasbourg, France
Philippe Schaeffer
Institut de Chimie de Strasbourg, Biogéochimie moléculaire
(UMR-7177), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 4 rue Blaise Pascal, 67000 Strasbourg, France
Laurent Hardion
Laboratoire Image Ville Environnement (UMR 7362), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de
l'Argonne, 67000 Strasbourg, France
Cécile Vittori
Laboratoire Image Ville Environnement (UMR 7362), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de
l'Argonne, 67000 Strasbourg, France
Stoil Chapkanski
Laboratoire de Géographie Physique (UMR-8591), Centre National de la Recherche Scientifique (CNRS)/ Université Paris 1,
Panthéon-Sorbonne, 1 Place Aristide Briand, 92195 Meudon, France
Hugo Delile
Laboratoire Archéorient (UMR-5133), Centre National de la
Recherche Scientifique (CNRS)/ Université de Lyon, MOM, 7 rue Raulin,
69007 Lyon, France
Laurent Schmitt
Laboratoire Image Ville Environnement (UMR 7362), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de
l'Argonne, 67000 Strasbourg, France
Frank Preusser
Institute of Earth and Environmental Sciences – Geology, University of Freiburg, Albertstr. 23b, 79104 Freiburg, Germany
Martine Trautmann
Laboratoire d'analyse des sols et des formations superficielles
(EOST-UMS-830), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de l'Argonne, 67000 Strasbourg, France
Alessia Masi
Dipartimento di Biologia Ambientale, Università degli Studi “La Sapienza” di Roma, Piazzale Aldo Moro 5, 00185 Rome, Italy
Cristiano Vignola
Dipartimento di Biologia Ambientale, Università degli Studi “La Sapienza” di Roma, Piazzale Aldo Moro 5, 00185 Rome, Italy
Laura Sadori
Dipartimento di Biologia Ambientale, Università degli Studi “La Sapienza” di Roma, Piazzale Aldo Moro 5, 00185 Rome, Italy
Jacob Morales
Departamento de Ciencias Históricas, Universidad de Las Palmas
de Gran Canaria, Calle Pérez del Toro, 1, Las Palmas de Gran Canaria
35003, Las Palmas, Spain
Paloma Vidal Matutano
Departamento de Ciencias Históricas, Universidad de Las Palmas
de Gran Canaria, Calle Pérez del Toro, 1, Las Palmas de Gran Canaria
35003, Las Palmas, Spain
Université Côte-d'Azur, CEPAM, CNRS, 24 Avenue des Diables
Bleus, 06000 Nice, France
Vincent Robin
Laboratoire Interdisciplinaire des environnements continentaux
(UMR-7360), Centre National de la Recherche Scientifique (CNRS)/Université de Lorraine, Campus Bridoux, Rue du Général
Delestraint, 57070 Metz, France
Benjamin Keller
Laboratoire Image Ville Environnement (UMR 7362), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de
l'Argonne, 67000 Strasbourg, France
Ángel Sanchez Bellón
Departamento de Ciencias de la Tierra, UGEA-PHAM, Universidad de
Cádiz, Avda. República Saharahui s/n, Campus Rio San Pedro, Puerto
Real, 11510 Cádiz, Spain
Javier Martínez López
Departamento de Ciencias de la Tierra, UGEA-PHAM, Universidad de
Cádiz, Avda. República Saharahui s/n, Campus Rio San Pedro, Puerto
Real, 11510 Cádiz, Spain
Gilles Rixhon
Laboratoire Image Ville Environnement (UMR 7362), Centre National de la Recherche Scientifique (CNRS)/Université de Strasbourg, 3 rue de
l'Argonne, 67000 Strasbourg, France
Ecole Nationale du Génie de l'Eau et de l'Environnement de
Strasbourg (ENGEES), 1 Quai Koch, 67000 Strasbourg, France
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Lake Ohrid is considered to be the oldest existing lake in Europe. Moreover, it has a very high degree of endemic biodiversity. During a drilling campaign at Lake Ohrid in 2013, a 569 m long sediment sequence was recovered from Lake Ohrid. The ongoing studies of this record provide first important information on the environmental and evolutionary history of the lake and the reasons for its high endimic biodiversity.
Odile Peyron, Nathalie Combourieu-Nebout, David Brayshaw, Simon Goring, Valérie Andrieu-Ponel, Stéphanie Desprat, Will Fletcher, Belinda Gambin, Chryssanthi Ioakim, Sébastien Joannin, Ulrich Kotthoff, Katerina Kouli, Vincent Montade, Jörg Pross, Laura Sadori, and Michel Magny
Clim. Past, 13, 249–265, https://doi.org/10.5194/cp-13-249-2017, https://doi.org/10.5194/cp-13-249-2017, 2017
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Giovanni Zanchetta, Eleonora Regattieri, Biagio Giaccio, Bernd Wagner, Roberto Sulpizio, Alex Francke, Hendrik Vogel, Laura Sadori, Alessia Masi, Gaia Sinopoli, Jack H. Lacey, Melanie J. Leng, and Niklas Leicher
Biogeosciences, 13, 2757–2768, https://doi.org/10.5194/bg-13-2757-2016, https://doi.org/10.5194/bg-13-2757-2016, 2016
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Chronology is fundamental in paleoclimatology for understanding timing of events and their origin. In this paper we try to obtain a more detailed chronology for the interval comprised between ca. 140 and 70 ka for the DEEP core in Lake Ohrid using regional independently-dated archives (i.e. speleothems and/or lacustrine succession with well-dated volcanic layers). This allows to insert the DEEP chronology within a common chronological frame between different continental and marine proxy records.
Laura Sadori, Andreas Koutsodendris, Konstantinos Panagiotopoulos, Alessia Masi, Adele Bertini, Nathalie Combourieu-Nebout, Alexander Francke, Katerina Kouli, Sébastien Joannin, Anna Maria Mercuri, Odile Peyron, Paola Torri, Bernd Wagner, Giovanni Zanchetta, Gaia Sinopoli, and Timme H. Donders
Biogeosciences, 13, 1423–1437, https://doi.org/10.5194/bg-13-1423-2016, https://doi.org/10.5194/bg-13-1423-2016, 2016
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Lake Ohrid (FYROM/Albania) is the deepest, largest and oldest lake in Europe. To understand the climatic and environmental evolution of its area, a palynological study was undertaken for the last 500 ka. We found a correspondence between forested/non-forested periods and glacial-interglacial cycles of marine isotope stratigraphy. Our record shows a progressive change from cooler and wetter to warmer and dryer interglacial conditions. This shift is also visible in glacial vegetation.
Alexander Francke, Bernd Wagner, Janna Just, Niklas Leicher, Raphael Gromig, Henrike Baumgarten, Hendrik Vogel, Jack H. Lacey, Laura Sadori, Thomas Wonik, Melanie J. Leng, Giovanni Zanchetta, Roberto Sulpizio, and Biagio Giaccio
Biogeosciences, 13, 1179–1196, https://doi.org/10.5194/bg-13-1179-2016, https://doi.org/10.5194/bg-13-1179-2016, 2016
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Clim. Past, 12, 51–73, https://doi.org/10.5194/cp-12-51-2016, https://doi.org/10.5194/cp-12-51-2016, 2016
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In this paper we use two climate models to test how Earth’s vegetation responded to changes in climate over the last 120 000 years, looking at warm interglacial climates like today, cold ice-age glacial climates, and intermediate climates. The models agree well with observations from pollen, showing smaller forested areas and larger desert areas during cold periods. Forests store most terrestrial carbon; the terrestrial carbon lost during cold climates was most likely relocated to the oceans.
B. Giaccio, E. Regattieri, G. Zanchetta, B. Wagner, P. Galli, G. Mannella, E. Niespolo, E. Peronace, P. R. Renne, S. Nomade, G. P. Cavinato, P. Messina, A. Sposato, C. Boschi, F. Florindo, F. Marra, and L. Sadori
Sci. Dril., 20, 13–19, https://doi.org/10.5194/sd-20-13-2015, https://doi.org/10.5194/sd-20-13-2015, 2015
Short summary
Short summary
As a pilot study for a possible depth-drilling project, an 82m long sedimentary succession was retrieved from the Fucino Basin, central Apennines, which hosts ca. 900m of lacustrine sediments. The acquired paleoclimatic record, from the retrieved core, spans the last 180ka and reveals noticeable variations related to the last two glacial-interglacial cycles. In light of these results, the Fucino sediments are likely to provide one of the longest continuous record for the last 2Ma.
M. Magny, N. Combourieu-Nebout, J. L. de Beaulieu, V. Bout-Roumazeilles, D. Colombaroli, S. Desprat, A. Francke, S. Joannin, E. Ortu, O. Peyron, M. Revel, L. Sadori, G. Siani, M. A. Sicre, S. Samartin, A. Simonneau, W. Tinner, B. Vannière, B. Wagner, G. Zanchetta, F. Anselmetti, E. Brugiapaglia, E. Chapron, M. Debret, M. Desmet, J. Didier, L. Essallami, D. Galop, A. Gilli, J. N. Haas, N. Kallel, L. Millet, A. Stock, J. L. Turon, and S. Wirth
Clim. Past, 9, 2043–2071, https://doi.org/10.5194/cp-9-2043-2013, https://doi.org/10.5194/cp-9-2043-2013, 2013
N. Combourieu-Nebout, O. Peyron, V. Bout-Roumazeilles, S. Goring, I. Dormoy, S. Joannin, L. Sadori, G. Siani, and M. Magny
Clim. Past, 9, 2023–2042, https://doi.org/10.5194/cp-9-2023-2013, https://doi.org/10.5194/cp-9-2023-2013, 2013
L. Sadori, E. Ortu, O. Peyron, G. Zanchetta, B. Vannière, M. Desmet, and M. Magny
Clim. Past, 9, 1969–1984, https://doi.org/10.5194/cp-9-1969-2013, https://doi.org/10.5194/cp-9-1969-2013, 2013
O. Peyron, M. Magny, S. Goring, S. Joannin, J.-L. de Beaulieu, E. Brugiapaglia, L. Sadori, G. Garfi, K. Kouli, C. Ioakim, and N. Combourieu-Nebout
Clim. Past, 9, 1233–1252, https://doi.org/10.5194/cp-9-1233-2013, https://doi.org/10.5194/cp-9-1233-2013, 2013
Related subject area
Location/Setting: Shelf | Subject: Geology | Geoprocesses: Geohazards
A roadmap for amphibious drilling at the Campi Flegrei caldera: insights from a MagellanPlus workshop
Marco Sacchi, Giuseppe De Natale, Volkhard Spiess, Lena Steinmann, Valerio Acocella, Marta Corradino, Shanaka de Silva, Alessandro Fedele, Lorenzo Fedele, Nobuo Geshi, Christopher Kilburn, Donatella Insinga, Maria-José Jurado, Flavia Molisso, Paola Petrosino, Salvatore Passaro, Fabrizio Pepe, Sabina Porfido, Claudio Scarpati, Hans-Ulrich Schmincke, Renato Somma, Mari Sumita, Stella Tamburrino, Claudia Troise, Mattia Vallefuoco, and Guido Ventura
Sci. Dril., 26, 29–46, https://doi.org/10.5194/sd-26-29-2019, https://doi.org/10.5194/sd-26-29-2019, 2019
Short summary
Short summary
A MagellanPlus workshop was held in Naples, Italy (25–28 February 2017), to explore the potential of the Campi Flegrei caldera as a target for an Amphibious Drilling Proposal to be submitted to international drilling programs. Campi Flegrei is an ideal natural laboratory to analyze the mechanisms of caldera dynamics and the relationships between hydrothermal and magmatic processes. The results will significantly advance our understanding of the most complex forms of volcanic structures on Earth.
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Short summary
PalaeoCADIX-Z is an interdisciplinary project that studied three cores drilled in a marine palaeochannel that ran through the ancient city of Cádiz (Spain). These cores reveal a ≥ 50 m thick Holocene sedimentary sequence. Importantly, most of the deposits date from the 1st millennium BCE to the 1st millennium CE. Geoarchaeologists, geomorphologists, archaeologists, sedimentologists, palaeoenvironmentalists, geochemists, and geochronologists collaborated within this project.
PalaeoCADIX-Z is an interdisciplinary project that studied three cores drilled in a marine...
