Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Kasia K. Sliwinska"'
Sea surface temperature evolution of the North Atlantic Ocean across the Eocene-Oligocene Transition
Autor:
Kasia K. Sliwinska, David K. Hutchinson, Devika Varma, Tirza Weitkamp, Emma Sheldon, Diederik Liebrand, Helen K. Coxall, Agatha M. de Boer, Stefan Schouten
When a permanent ice cap developed on Antarctica during the Eocene–Oligocene transition (EOT; ~34.44 to 33.65 million years ago (Ma)), Earth witnessed a transition from a greenhouse towards a glacially driven climate. Evidence of high-latitude cool
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0610c2a11fbb5ecbf22a9e7121bdafff
https://doi.org/10.5194/egusphere-egu23-8831
https://doi.org/10.5194/egusphere-egu23-8831
Autor:
Kasia K. Śliwińska, Thomas Denk, Karen Dybkjær, Julie Margrethe Fredborg, Sofie Lindström, Stefan Piasecki, Erik Skovbjerg Rasmussen
Publikováno v:
GEUS Bulletin, Vol 57, Pp 1-18 (2024)
Despite often being referred to as a ‘coolhouse climate’, the climate during the Miocene (23.03–5.33 Ma) was overall humid, warm and temperate. It was paced by orbitally driven cooler periods (the Oligocene–Miocene Transition and Mi-events) o
Externí odkaz:
https://doaj.org/article/a29413fe195142e3a60b91b012583b74
Autor:
Erik S. Rasmussen, Karen Dybkjær, Jørgen A. Bojesen-Koefoed, Nicolas Thibault, Kasia K. Sliwinska, Caroline H Lear, Timothy D Herbert, Madeleine L. Vickers, Emil Munck Soltau
The Miocene climate was dynamic, oscillating between major glaciation events and greenhouse conditions (the so-called Miocene Climatic Optimum or MCO). However, forcing factors responsible for climatic transitions from one state to another are not fu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f93762375177a3794915c458bde9b87a
https://doi.org/10.5194/egusphere-egu21-15183
https://doi.org/10.5194/egusphere-egu21-15183
Autor:
Jørgen A. Bojesen-Koefoed, Henrik Nøhr-Gansen, Kasia K. Sliwinska, Gunver Krarup Pedersen, David Naafs, Jussi Hovikovski, Paul Cornils Knutz
The super greenhouse climate of the middle Cretaceous represents an analogue for an extreme CO2 induced (run-away) climate system. In order to improve the understanding of how the high northern latitudes responded to the escalating middle Cretaceous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a56b1aa07de57947b87860a25b1eb711
https://doi.org/10.5194/egusphere-egu2020-18455
https://doi.org/10.5194/egusphere-egu2020-18455
Autor:
Claire E Huck, Alba Legarda-Lisarri, Agatha M. de Boer, Jan Backman, Tina van de Flierdt, Matthew Huber, James C Zachos, Helen K. Coxall, Kasia K. Sliwinska, Matt O'Regan, Caroline H Lear
Publikováno v:
Nature Geoscience. 11:190-196
The onset of the North Atlantic Deep Water formation is thought to have coincided with Antarctic ice-sheet growth about 34 million years ago (Ma). However, this timing is debated, in part due to questions over the geochemical signature of the ancient
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::650f657b923f46891cccb166d4a678e3
https://doi.org/10.1038/s41561-018-0069-9
https://doi.org/10.1038/s41561-018-0069-9
Autor:
Kasia K. Sliwinska, James C Zachos, Tina van de Flierdt, Claire E Huck, Jan Backman, Matt O'Regan, Caroline H Lear, Helen K. Coxall
Publikováno v:
Rendiconti online della Società Geologica Italiana. 31:48-49
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe9827ea67fc78c6ae0ef273ea5e42dc
https://doi.org/10.3301/rol.2014.39
https://doi.org/10.3301/rol.2014.39