Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Serginio R. C. Remmelzwaal"'
Autor:
Sietske J. Batenburg, Serginio R. C. Remmelzwaal, Stuart A. Robinson, Hugh C. Jenkyns, Andrew S. Gale, Lauren K. O'Connor, Ian J. Parkinson
Publikováno v:
O'Connor, L K, Jenkyns, H C, Robinson, S A, Remmelzwaal, S R C, Batenburg, S J, Parkinson, I J & Gale, A S 2020, ' A re-evaluation of the Plenus Cold Event, and the links between CO2, temperature, and seawater chemistry during OAE 2 ', Paleoceanography and Paleoclimatology, vol. 35, no. 4, e2019PA003631 . https://doi.org/10.1029/2019PA003631
Paleoceanography and Paleoclimatology
Paleoceanography and Paleoclimatology, American Geophysical Union, 2020, 35 (4), pp.e2019PA003631. ⟨10.1029/2019PA003631⟩
Paleoceanography and Paleoclimatology, 2020, 35 (4), pp.e2019PA003631. ⟨10.1029/2019PA003631⟩
Paleoceanography and Paleoclimatology
Paleoceanography and Paleoclimatology, American Geophysical Union, 2020, 35 (4), pp.e2019PA003631. ⟨10.1029/2019PA003631⟩
Paleoceanography and Paleoclimatology, 2020, 35 (4), pp.e2019PA003631. ⟨10.1029/2019PA003631⟩
International audience; The greenhouse world of the mid‐Cretaceous (~94 Ma) was punctuated by an episode of abrupt climatic upheaval: Oceanic Anoxic Event 2 (OAE 2). High‐resolution climate records reveal considerable changes in temperature, carb
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2e8b1760bd9e492046c7844236bfdb0f
https://doi.org/10.1029/2019pa003631
https://doi.org/10.1029/2019pa003631
Autor:
Yannick Donnadieu, Philip F Sexton, Serginio R. C. Remmelzwaal, Sophie Dixon, Caroline L. Peacock, Ian J. Parkinson, Daniela N. Schmidt, Fanny M. Monteiro, Manuela A. Fehr, Rachael H. James
Publikováno v:
Paleoceanography and Paleoclimatology
Paleoceanography and Paleoclimatology, American Geophysical Union, 2019, 34 (6), pp.917-929. ⟨10.1029/2018PA003372⟩
Paleoceanography and Paleoclimatology, 2019, 34 (6), pp.917-929. ⟨10.1029/2018PA003372⟩
Remmelzwaal, S, Dixon, S, Parkinson, I, Schmidt, D, Monteiro, F, Sexton, P F, Fehr, M A, Peacock, C, Donnadieu, Y & James, R 2019, ' Investigating Ocean Deoxygenation During the PETM Through the Cr Isotopic Signature of Foraminifera ', Paleoceanography and Paleoclimatology, vol. 34, no. 6, pp. 917-929 . https://doi.org/10.1029/2018PA003372
Paleoceanography and Paleoclimatology, American Geophysical Union, 2019, 34 (6), pp.917-929. ⟨10.1029/2018PA003372⟩
Paleoceanography and Paleoclimatology, 2019, 34 (6), pp.917-929. ⟨10.1029/2018PA003372⟩
Remmelzwaal, S, Dixon, S, Parkinson, I, Schmidt, D, Monteiro, F, Sexton, P F, Fehr, M A, Peacock, C, Donnadieu, Y & James, R 2019, ' Investigating Ocean Deoxygenation During the PETM Through the Cr Isotopic Signature of Foraminifera ', Paleoceanography and Paleoclimatology, vol. 34, no. 6, pp. 917-929 . https://doi.org/10.1029/2018PA003372
Over the past several decades, oxygen minimum zones have rapidly expanded due to rising temperatures raising concerns about the impacts of future climate change. One way to better understand the drivers behind this expansion is to evaluate the links
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9a46914edb0607a8aca66a2b6917e6ed
https://hal.archives-ouvertes.fr/hal-02902804
https://hal.archives-ouvertes.fr/hal-02902804
Autor:
Fanny M. Monteiro, Gordon N. Inglis, Serginio R. C. Remmelzwaal, Heather L. Buss, Paul J. Valdes, Marcus P. S. Badger, B. David A. Naafs, Alex Dickson, Alexander Farnsworth, Daniel J. Lunt, Megan Rohrssen, Matthew J. Carmichael, Richard D. Pancost, Leila Behrooz
Publikováno v:
Carmichael, M, Inglis, G, Badger, M, Naafs, D, Behrooz, L, Remmelzwaal, S, Monteiro, F, Rohrssen, M, Farnsworth, A, Buss, H, Dickson, A J, Valdes, P, Lunt, D & Pancost, R 2017, ' Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum ', Global and Planetary Change, vol. 157, pp. 114-138 . https://doi.org/10.1016/j.gloplacha.2017.07.014
The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal, ~56 million years ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. Characterised by surface temperature increases of between 5 – 9 °C and a rapid onset of less than
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e688e12bb5ee08edea146ae29c9eafb1
https://ora.ox.ac.uk/objects/uuid:3e41198a-3f6f-4d84-853c-e143dc3d480d
https://ora.ox.ac.uk/objects/uuid:3e41198a-3f6f-4d84-853c-e143dc3d480d