Articles | Volume 13, issue 12
https://doi.org/10.5194/cp-13-1901-2017
© Author(s) 2017. 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-13-1901-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The climate of the Common Era off the Iberian Peninsula
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
CCMAR, Centro de Ciências do Mar, Universidade do Algarve, Campus de
Gambelas, 8005-139 Faro, Portugal
Teresa Rodrigues
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
CCMAR, Centro de Ciências do Mar, Universidade do Algarve, Campus de
Gambelas, 8005-139 Faro, Portugal
Marta Rufino
CCMAR, Centro de Ciências do Mar, Universidade do Algarve, Campus de
Gambelas, 8005-139 Faro, Portugal
IFREMER – Centre Atlantique (French Research Institute for Exploitation
of the Sea), Département Ecologie et Modèles pour l'Halieutique
(EMH), Rue de l'Ile d'Yeu – BP 21105, 44311 Nantes CEDEX 3, France
Emília Salgueiro
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
CCMAR, Centro de Ciências do Mar, Universidade do Algarve, Campus de
Gambelas, 8005-139 Faro, Portugal
Dulce Oliveira
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
CCMAR, Centro de Ciências do Mar, Universidade do Algarve, Campus de
Gambelas, 8005-139 Faro, Portugal
Paléoclimatologie et paléoenvironnements marins, Université de Bordeaux, EPOC, UMR 5805, 33615 Pessac, France
Sandra Gomes
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
Paulo Oliveira
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
Ana Costa
Centro de Investigação em Biodiversidade e Recursos Genétics
(EnvArchCIBIO/InBIO) and Archaeosciences Laboratory (LARC/DGPC), Rua da Bica
do Marquês, 2, 1300-087 Lisbon, Portugal
Mário Mil-Homens
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
Teresa Drago
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
Instituto Dom Luiz, Universidade de Lisboa, 1749-016 Lisbon, Portugal
Filipa Naughton
Portuguese Institute for Sea and Atmosphere (IPMA), Divisão de
Geologia Marinha (DivGM), Rua Alferedo Magalhães Ramalho 6, 1495-006 Lisbon,
Portugal
CCMAR, Centro de Ciências do Mar, Universidade do Algarve, Campus de
Gambelas, 8005-139 Faro, Portugal
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Subject: Ocean Dynamics | Archive: Marine Archives | Timescale: Centennial-Decadal
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The response of the Peruvian Upwelling Ecosystem to centennial-scale global change during the last two millennia
The Impact of the Little Ice Age on Coccolithophores in the Central Mediterranea Sea
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H. Kuehn, L. Lembke-Jene, R. Gersonde, O. Esper, F. Lamy, H. Arz, G. Kuhn, and R. Tiedemann
Clim. Past, 10, 2215–2236, https://doi.org/10.5194/cp-10-2215-2014, https://doi.org/10.5194/cp-10-2215-2014, 2014
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Annually laminated sediments from the NE Bering Sea reveal a decadal-scale correlation to Greenland ice core records during termination I, suggesting an atmospheric teleconnection. Lamination occurrence is tightly coupled to Bølling-Allerød and Preboreal warm phases. Increases in export production, closely coupled to SST and sea ice changes, are hypothesized to be a main cause of deglacial anoxia, rather than changes in overturning/ventilation rates of mid-depth waters entering the Bering Sea.
R. Salvatteci, D. Gutiérrez, D. Field, A. Sifeddine, L. Ortlieb, I. Bouloubassi, M. Boussafir, H. Boucher, and F. Cetin
Clim. Past, 10, 715–731, https://doi.org/10.5194/cp-10-715-2014, https://doi.org/10.5194/cp-10-715-2014, 2014
A. Incarbona, P. Ziveri, E. Di Stefano, F. Lirer, G. Mortyn, B. Patti, N. Pelosi, M. Sprovieri, G. Tranchida, M. Vallefuoco, S. Albertazzi, L. G. Bellucci, A. Bonanno, S. Bonomo, P. Censi, L. Ferraro, S. Giuliani, S. Mazzola, and R. Sprovieri
Clim. Past, 6, 795–805, https://doi.org/10.5194/cp-6-795-2010, https://doi.org/10.5194/cp-6-795-2010, 2010
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Short summary
Reconstructions of the last 2000-year climatic conditions along the Iberian Margin, a vulnerable region regarding current global warming, reveal a long-term cooling in sea surface temperature (SST) ending with the 19th century and centennial-scale variability that exposes warm SSTs throughout the first 1300 years followed by the colder Little Ice Age. The Industrial Era starts by 1800 CE, with an SST rise and a second increase in SST at ca. 1970 CE, particularly marked in the southern region.
Reconstructions of the last 2000-year climatic conditions along the Iberian Margin, a vulnerable...