Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Franziska Tell"'
Autor:
Mohamed Ezat, Julie Meilland, Adele Westgård, Thomas Chalk, Freya Sykes, Naima El Bani Altuna, Pushpak Nadar, Franziska Tell, Elwyn De la Vega
Publikováno v:
CAGE – Centre for Arctic Gas Hydrate, Environment and Climate Report Series; Vol. 10 (2022)
From the morning of June 23rd to the morning of June 30th 2022, the Department of Geosciences at UiT the Arctic University of Norway, arranged a scientific cruise on R/V “Helmer Hanssen aimed at sampling living planktic foraminifera (Neogloboquadri
With ongoing warming and sea ice loss, the Arctic Ocean and its marginal seas as a habitat for pelagic calcifiers are changing, possibly resulting in modifications of the regional carbonate cycle and the composition of the seafloor sediment. A substa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e605383955c2b91f6cf7f254c3d295f1
https://bg.copernicus.org/articles/19/4903/2022/
https://bg.copernicus.org/articles/19/4903/2022/
With ongoing warming and sea ice loss, the Arctic Ocean and its marginal seas will likely become more hospitable to pelagic calcifiers, resulting in modifications of the regional carbonate cycle and the composition of the seafloor sediment. A substan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a8ecf6253a675058d398501a23e35d1e
https://bg.copernicus.org/preprints/bg-2022-59/
https://bg.copernicus.org/preprints/bg-2022-59/
Planktonic foraminifera, marine protists and calcifiers, are globally responsible for about one quarter of the global pelagic calcite flux, but their contribution to it in the subarctic and Arctic realm has not been fully resolved. With ongoing warmi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1757e4af78a35a17353c114652b39bb9
https://doi.org/10.5194/egusphere-egu22-1589
https://doi.org/10.5194/egusphere-egu22-1589
Autor:
Franziska Tell, Bénédicte Minster, Henning Kuhnert, Dan Hammarlund, Ulrich von Grafenstein, Inga Labuhn
Publikováno v:
Biogeosciences
Biogeosciences, 2022, 19 (11), pp.2759-2777. ⟨10.5194/bg-19-2759-2022⟩
Biogeosciences, 2022, 19 (11), pp.2759-2777. ⟨10.5194/bg-19-2759-2022⟩
Carbonate shells and encrustations from lacustrine organisms provide proxy records of past environmental and climatic changes. The carbon isotopic composition (δ13C) of such carbonates depends on the δ13C of dissolved inorganic carbon (DIC). Their
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::22fdbca2bb97b3ae5c12844ea7f911ab
https://doi.org/10.5194/egusphere-egu21-13178
https://doi.org/10.5194/egusphere-egu21-13178