Zobrazeno 1 - 10
of 375
pro vyhledávání: '"Lysocline"'
Autor:
Miloš Milovančević, Petra Karanikić
Publikováno v:
Journal of Radioanalytical and Nuclear Chemistry. 330:1037-1043
The study's major goal was to identify the most significant coccoliths based on foraminiferal species and fragment abundances, oxygen isotope ratios, and calculated temperatures. The degree of preservation of coccoliths and foraminifera indicates tha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5164ea661124863cbeb134380dd63e5
https://doi.org/10.1007/s10967-021-08044-9
https://doi.org/10.1007/s10967-021-08044-9
Publikováno v:
Geoscience Frontiers, Vol 12, Iss 2, Pp 521-530 (2021)
Early Eocene hyperthermals are geologically short-lived global warming events and represent fundamental perturbations to the global carbon cycle and the Earth’s ecosystem due to massive additions of isotopically light carbon to the ocean-atmosphere
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::419a9152e90d2735b1bedd033dd86838
https://doi.org/10.1016/j.gsf.2020.07.014
https://doi.org/10.1016/j.gsf.2020.07.014
Publikováno v:
Acta Oceanologica Sinica. 40:155-161
Site U1446 (19°50′N, 85°44′E, at water depth 1 430 m) was drilled during Expedition 353 (Indian monsoon rainfall) of the International Ocean Discovery Program (IODP). It is located in the Mahanadi offshore basin, on the northern Bay of Bengal.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1de96560674acceaf931a6b4d9744305
https://doi.org/10.1007/s13131-021-1821-3
https://doi.org/10.1007/s13131-021-1821-3
Publikováno v:
Annual Review of Marine Science. 13:57-80
The dissolution of CaCO3 minerals in the ocean is a fundamental part of the marine alkalinity and carbon cycles. While there have been decades of work aimed at deriving the relationship between dissolution rate and mineral saturation state (a so-call
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa2b14689b7adcdc607af797842535de
https://doi.org/10.1146/annurev-marine-041720-092514
https://doi.org/10.1146/annurev-marine-041720-092514
Akademický článek
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Autor:
Ekaterina Ovsepyan, Elena Ivanova
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 514:349-360
The Atlantic Meridional Overturning Circulation (AMOC) is a key component of the global climate system due to its role in oceanic heat transport, CO2 exchange between the ocean and atmosphere, and carbon storage in the ocean interior. Previous studie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ccac4379720e68dcd3bd8489e25e1470
https://doi.org/10.1016/j.palaeo.2018.10.031
https://doi.org/10.1016/j.palaeo.2018.10.031
Autor:
Leech, Peter Joseph
The shape of the thermocline and the depth of the lysoline in the western tropical Pacific are both influenced by the overlying atmosphere, and both the shape of thermocline and the depth of the lysocline can be reconstructed from foraminifera-based
Externí odkaz:
http://hdl.handle.net/1853/49029
Akademický článek
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Autor:
Elizabeth D. Swanner, Mojtaba Fakhraee, Amy Myrbo, Sergei Katsev, Simon W. Poulton, Ashley Grengs, Andrew W. Bray, Chad Wittkop, Nicholas Lambrecht
Most manganese (Mn) enrichments in the sedimentary rock record are hosted in carbonate minerals, which are assumed to have formed by diagenetic reduction of precursor Mn-oxides, and are considered diagnostic of strongly oxidizing conditions. Here we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cd9346fefd9c53ccd492fc1e09307d8e
https://eprints.whiterose.ac.uk/157891/1/wittkop_etal_2020_EPSL_preprint.pdf
https://eprints.whiterose.ac.uk/157891/1/wittkop_etal_2020_EPSL_preprint.pdf
Publikováno v:
Journal of Sedimentary Environments. 3:280-289
Planktonic foraminifera inhabit in the ocean waters and their spatial distribution is driven mainly by surface temperature. Thus, the tests remain deposited in the ocean sediment show different assemblages according to global climate zones. The main
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c079888bfa072d5c841e3a2caa34665b
https://doi.org/10.12957/jse.2018.39156
https://doi.org/10.12957/jse.2018.39156