Zobrazeno 1 - 10
of 41
pro vyhledávání: '"Gianluca, Marino"'
Autor:
Hsun-Ming Hu, Gianluca Marino, Carlos Pérez-Mejías, Christoph Spötl, Yusuke Yokoyama, Jimin Yu, Eelco Rohling, Akihiro Kano, Patrick Ludwig, Joaquim G. Pinto, Véronique Michel, Patricia Valensi, Xin Zhang, Xiuyang Jiang, Horng-Sheng Mii, Wei-Yi Chien, Hsien-Chen Tsai, Wen-Hui Sung, Chia-Hao Hsu, Elisabetta Starnini, Marta Zunino, Chuan-Chou Shen
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-11 (2024)
Abstract The Marine Isotope Stage (MIS) 11c interglacial and its preceding glacial termination represent an enigmatically intense climate response to relatively weak insolation forcing. So far, a lack of radiometric age control has confounded a detai
Externí odkaz:
https://doaj.org/article/e974bcb9c78b4745ae494c4bc9db4d69
Autor:
Savannah, Myers, Eelco, Rohling, Timme, Donders, Katharine, Grant, Jörg, Keller, Gianluca, Marino, Francesca, Sangiorgi, Francesca, Caridi, Caterina, Morigi, Anna, Sabbatini, Alessandra, Negri
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 15 September 2024 650
Autor:
Eelco J. Rohling, Fiona D. Hibbert, Katharine M. Grant, Eirik V. Galaasen, Nil Irvalı, Helga F. Kleiven, Gianluca Marino, Ulysses Ninnemann, Andrew P. Roberts, Yair Rosenthal, Hartmut Schulz, Felicity H. Williams, Jimin Yu
Publikováno v:
Nature Communications, Vol 10, Iss 1, Pp 1-9 (2019)
The relative contributions of the Greenland and Antarctic Ice Sheets to Last Interglacial sea level rise remain debated, as do the timing and magnitude. Here, data show that the Antarctic Ice Sheet dominated particularly high levels of sea-level rise
Externí odkaz:
https://doaj.org/article/e20a20a211e24487bbf968302680e299
Autor:
Alessandro Incarbona, Gianluca Marino, Enrico Di Stefano, Michael Grelaud, Nicola Pelosi, Laura Rodríguez-Sanz, Eelco J. Rohling
Publikováno v:
Universitat Autònoma de Barcelona
Altres ajuts: Unidad de excelencia María de Maeztu CEX2019-000940-M; Universidade de Vigo's programme to attract excellent research talent (RR04092017) The eastern Mediterranean Sea lies under the influence of high- and low-latitude climatic systems
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7d1e7248829ae506bacb0199e2be2609
https://ddd.uab.cat/record/266905
https://ddd.uab.cat/record/266905
Autor:
Emmeline Gray, Anta-Clarisse Sarr, Gianluca Marino, Eelco J. Rohling, Julia Lübbers, Kazuyo Tachikawa, Ann Holbourn, Nils Andersen, Wolfgang Kuhnt, Clara T Bolton, Katharine M. Grant
Publikováno v:
Climate of the Past
Climate of the Past, 2022, 18, pp.713-738. ⟨10.5194/cp-18-713-2022⟩
Climate of the Past, 2022, 18, pp.713-738. ⟨10.5194/cp-18-713-2022⟩
In the modern northern Indian Ocean, biological productivity is intimately linked to near-surface oceanographic dynamics forced by the South Asian, or Indian, monsoon. In the late Pleistocene, this strong seasonal signal is transferred to the sedimen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5062961bff0bafb51cd7154be2755230
https://hal.science/hal-03384903
https://hal.science/hal-03384903
Publikováno v:
Paleoceanography and Paleoclimatology. 34:1487-1516
Organic-rich sapropel layers punctuate the eastern Mediterranean sedimentary sequence, recording deep-sea anoxic events. The timing of sapropel deposition coincides with precession minima, which are associated with the northward migration of the mons
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a421158c21726164b77c173be84f9477
https://doi.org/10.1029/2019pa003652
https://doi.org/10.1029/2019pa003652
Autor:
Clara T. Bolton, Emmeline Gray, Wolfgang Kuhnt, Ann E. Holbourn, Julia Lübbers, Katharine Grant, Kazuyo Tachikawa, Gianluca Marino, Eelco J. Rohling, Anta-Clarisse Sarr, Nils Andersen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9a472970c36a878f9cfe4c01ce63f12f
https://doi.org/10.5194/cp-2021-77-supplement
https://doi.org/10.5194/cp-2021-77-supplement
Autor:
Gianluca Marino, Gianluca Sottili, Hervé Guillou, Sébastien Nomade, Danilo M. Palladino, Fabrizio Marra, Alison Pereira, Lorenzo Monaco, Niklas Leicher, Mario Gaeta, Biagio Giaccio, Vincent Scao, Giovanni Zanchetta
Publikováno v:
Quaternary Science Reviews
Quaternary Science Reviews, Elsevier, 2021, 263, pp.106976. ⟨10.1016/j.quascirev.2021.106976⟩
Quaternary Science Reviews, 2021, 263, pp.106976. ⟨10.1016/j.quascirev.2021.106976⟩
Quaternary Science Reviews, Elsevier, 2021, 263, pp.106976. ⟨10.1016/j.quascirev.2021.106976⟩
Quaternary Science Reviews, 2021, 263, pp.106976. ⟨10.1016/j.quascirev.2021.106976⟩
International audience; Glacial-interglacial variations in ice volume and sea level are essential components of the Pleistocene global climate evolution. Deciphering the timing of change of these key climate parameters with respect to the insolation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8697e115dcd232cfae343896d8d10992
http://hdl.handle.net/11573/1548271
http://hdl.handle.net/11573/1548271
Autor:
Liang Chen, Andrew P. Roberts, Laura Rodríguez-Sanz, David Heslop, Gianluca Marino, Helen McGregor, Eelco J. Rohling, Xiang Zhao, Heiko Pälike, Liao Chang
Publikováno v:
Geochemistry, Geophysics, Geosystems. 18:1435-1450
Relative paleointensity (RPI) variations of Earth's magnetic field are widely used to understand geomagnetic field behavior and to develop age models for sedimentary sequences. RPI estimation is based on a series of assumptions. One key assumption th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3741da432ec58c9078c600fa808bbb2d
https://doi.org/10.1002/2016gc006753
https://doi.org/10.1002/2016gc006753
Autor:
Eirik Vinje Galaasen, Helga F Kleiven, Eelco J. Rohling, Yair Rosenthal, Katharine M. Grant, Gianluca Marino, Andrew P. Roberts, Fiona D. Hibbert, Felicity Williams, Nil Irvali, Hartmut Schulz, Jimin Yu, Ulysses S Ninnemann
Publikováno v:
Nature Communications
Nature Communications, Vol 10, Iss 1, Pp 1-9 (2019)
Nature Communications, Vol 10, Iss 1, Pp 1-9 (2019)
The last interglacial (LIG; ~130 to ~118 thousand years ago, ka) was the last time global sea level rose well above the present level. Greenland Ice Sheet (GrIS) contributions were insufficient to explain the highstand, so that substantial Antarctic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bc44489abfd77f2f876ad5d5645d64ba
https://hdl.handle.net/1956/23808
https://hdl.handle.net/1956/23808