Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Peter Bijl"'
Understanding the extreme greenhouse of the Eocene (56–34Ma ago) is key to anticipate potential future conditions. During the Eocene, the Antarctic continent remained mostly ice-free despite large temperature swings. Seemingly contradictory indicat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c46140358189769fab1839e8b2c22316
https://doi.org/10.5194/cp-2023-36
https://doi.org/10.5194/cp-2023-36
Preliminary examination of the biomarker composition of Paleocene to Campanian (~63-74 Ma) organic-rich sediments recovered from the Transkei Basin (Hole U1581B; 35° 41’S, 29° 39’E), offshore South Africa, during IODP Expedition 392 reveals sui
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0bf2a02726ab3ab87683ae8810ab1a68
https://doi.org/10.5194/egusphere-egu23-10010
https://doi.org/10.5194/egusphere-egu23-10010
Autor:
Dominique Jenny, Evalien Baas, Wouter Stouthamer, Jakub Witkowski, Isabella Raffi, Peter Bijl, Francien Peterse, Appy Sluijs
The Oligocene (33.9 – 23.03 Ma ago) and early Miocene (23.03 – 19 Ma) experienced large climate and ice sheet fluctuations in a most likely unipolar icehouse, with glaciation limited to the Southern Hemisphere. This time interval provides a usefu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e00d75632bc0b6eef9c2984fc56fd7d5
https://doi.org/10.5194/egusphere-egu23-12176
https://doi.org/10.5194/egusphere-egu23-12176
Autor:
Suning Hou, Malte Stockhausen, Leonie Toebrock, Francesca Sangiorgi, Aidan Starr, Melissa Berke, Martin Ziegler, Peter Bijl
The mid-Pliocene (3.3-3.0 Ma) is a time when the Earth's climate fluctuated between cold glacial conditions (marine isotope stage M2; 3.3 Ma) and periods when global temperatures were ~3°C warmer than the pre-industrial (Mid-Pliocene warm period; 3.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::635346f2bd36b04afde529914c05d99e
https://doi.org/10.5194/egusphere-egu23-7924
https://doi.org/10.5194/egusphere-egu23-7924
During the Cenozoic (66–0 Ma) Tasmania has continuously been at a crucial geographic location. It represented the final tectonic connection between Australia and Antarctica before complete separation of both continents in the late Eocene, and there
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b5a99a7db67b57b19e78e601f1b0139c
https://doi.org/10.5194/egusphere-egu23-2802
https://doi.org/10.5194/egusphere-egu23-2802
Autor:
Chris Fokkema, Tobias Agterhuis, Liam Kelly, Agnese Mannucci, Basse Theijse, Or Bialik, Peter Bijl, Henk Brinkhuis, Gerald Dickens, Simone Galeotti, Francien Peterse, Appy Sluijs
Rapid climatic and carbon cycle upheavals in the early Eocene have been of strong interest for the past decades. Multiple of these events represent global warming events (i.e. hyperthermals), including the Paleocene Eocene Thermal Maximum (PETM; 56 M
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9dcdb0af3d3f61d0170cedd9a55ccb13
https://doi.org/10.5194/egusphere-egu23-16165
https://doi.org/10.5194/egusphere-egu23-16165
High latitude warmth during the Eocene greenhouse climate has posed many challenges for climate modelling studies. Recent improvements in both the proxy records and model simulations are bringing these closer together, particularly regarding the meri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3dc6fc4c00a37c8a0e0585dc2b59bfaf
https://doi.org/10.5194/egusphere-egu23-16108
https://doi.org/10.5194/egusphere-egu23-16108
Autor:
Joost Frieling, Steve Bohaty, Margot Cramwinckel, Tammo Reichgelt, Stephen Gallagher, Guy Holdgate, Francien Peterse, Jörg Pross, Appy Sluijs, Peter Bijl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0453dd1e16dda2054e940b634a804300
https://doi.org/10.1002/essoar.10512373.1
https://doi.org/10.1002/essoar.10512373.1
Autor:
Frida Hoem, Isabel Sauermilch, Adam Aleksinski, Matthew Huber, Francien Peterse, Francesca Sangiorgi, Peter Bijl
Large Oligocene Antarctic ice sheets co-existed with warm adjacent ocean waters. To provide a broad Southern Ocean perspective to such warmth, we reconstruct the strength and variability of the Oligocene Australian-Antarctic latitudinal sea surface t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9fadbc57a7d9a5c0be7d9134067f69c1
https://doi.org/10.21203/rs.3.rs-1516446/v1
https://doi.org/10.21203/rs.3.rs-1516446/v1