Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Elaine M. Mawbey"'
Autor:
Chen-Feng You, Shuang Zhang, William R Gray, John R. Kucklick, Laura F. Robinson, Joseph A. Stewart, James W. B. Rae, Freya Hemsing, Thomas B Chalk, Arnaud Dapoigny, Russell D. Day, Philip Holdship, Michael J. Henehan, Eric Douville, Rachael Shuttleworth, Ana Kolevica, Marcus Gutjahr, Elaine M. Mawbey, Rosanna Greenop, Gavin L. Foster, Steven J. Christopher, Yen-Po Lin, Yu-Te Hsieh, Louise Bordier
Publikováno v:
Geostandards and Geoanalytical Research
Geostandards and Geoanalytical Research, 2021, 45, pp.77-96. ⟨10.1111/ggr.12363⟩
Geostandards and Geoanalytical Research, Wiley, 2021, 45, pp.77-96. ⟨10.1111/ggr.12363⟩
Geostandards and Geoanalytical Research, 2021, 45, pp.77-96. ⟨10.1111/ggr.12363⟩
Geostandards and Geoanalytical Research, Wiley, 2021, 45, pp.77-96. ⟨10.1111/ggr.12363⟩
Boron isotopes and trace element content measurements were funded by: the French National Research Agency projects ANR CARBORIC (Grant No. ANR-13-BS06-0013-04) and ANR HAMOC (Grant No. ANR-13-BS06-0003-02) at LSCE; NERC NE/N003861/1 & NE/S001743/1 at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c0b53fa301749f09398c74da176e1058
https://hdl.handle.net/10023/21147
https://hdl.handle.net/10023/21147
Autor:
Elaine M. Mawbey, Sindia M. Sosdian, Katharina Billups, Rosalind E. M. Rickaby, Liselotte Diester-Haass, Caroline H Lear
The ~100 k.y. cyclicity of the late Pleistocene ice ages started during the mid-Pleistocene transition (MPT), as ice sheets became larger and persisted for longer. The climate system feedbacks responsible for introducing this nonlinear ice sheet resp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eb91a19f3e8ba954b50cf6d5747b6f52
https://orca.cardiff.ac.uk/id/eprint/95508/1/Geology-2016-Lear-G38636.1.pdf
https://orca.cardiff.ac.uk/id/eprint/95508/1/Geology-2016-Lear-G38636.1.pdf
Autor:
Caroline H Lear, Elaine M. Mawbey
Publikováno v:
Geology. 41:963-966
Ice sheet models suggest that once formed, the large, high-\ud altitude East Antarctic Ice Sheet was relatively self-stabilizing, due to its cold upper surface. The ice sheet hysteresis problem results from an inability to reconcile this expectation
Publikováno v:
Paleoceanography. 25
The sensitivities of benthic foraminiferal Mg/Ca and Li/Ca to bottom water temperature and carbonate saturation state have recently been assessed. Here we present a new approach that uses paired Mg/Ca and Li/Ca records to calculate simultaneous chang