Zobrazeno 1 - 10
of 241
pro vyhledávání: '"C, Bova"'
Autor:
V. J. Lawson, Y. Rosenthal, S. C. Bova, J. Lambert, B. K. Linsley, K. Bu, V. J. Clementi, A. Elmore, E. L. McClymont
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 8, Pp n/a-n/a (2024)
Abstract Boron to calcium (B/Ca) records in benthic foraminifera, used for reconstructing the carbonate ion saturation state (ΔCO3) of the deep ocean, suggest that carbon sequestration in the Southern Pacific contributed to lowering atmospheric CO2
Externí odkaz:
https://doaj.org/article/5d65720fa25a4fdcaf8c537c1fedad43
Publikováno v:
Earth System Science Data, Vol 16, Pp 701-713 (2024)
The Western Pacific Warm Pool (WPWP) exhibits different glacial–interglacial climate variability compared to high latitudes, and its sea surface temperatures are thought to respond primarily to changes in greenhouse forcing. To better characterize
Externí odkaz:
https://doaj.org/article/5f7bf1c80257470eae81a29ad53442c3
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 16, Pp n/a-n/a (2023)
Abstract Despite small direct changes to radiative forcing, solar sunspot cycles are observed in climate records because of climate system amplification that primarily affects wind and precipitation belts. We present a proxy record resolving the domi
Externí odkaz:
https://doaj.org/article/4a7bb1fadbe141e59d1f7ed22eba3200
Autor:
Vincent J. Clementi, Yair Rosenthal, Samantha C. Bova, Elizabeth K. Thomas, James D. Wright, Richard A. Mortlock, Owen C. Cowling, Linda V. Godfrey, Laurel B. Childress, Expedition 379T Scientists
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-9 (2022)
Freshening of porewater in marine sediments offshore the southern Chilean Margin is driven by submarine emplacement of fossil groundwater below Patagonia, according to elemental and isotopic analyses of sedimentary pore waters.
Externí odkaz:
https://doaj.org/article/680fc77f075144648690c748e302b529
Autor:
Chen Li, Vincent J. Clementi, Samantha C. Bova, Yair Rosenthal, Laurel B. Childress, James D. Wright, Zhimin Jian, Expedition 379T Scientists
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 9, Pp n/a-n/a (2022)
Abstract Sediment cores recently collected from the Chilean Margin during D/V JOIDES Resolution Expedition 379T (JR100) document variability in shipboard‐generated records of the green/blue (G/B) ratio. These changes show a strong coherence with be
Externí odkaz:
https://doaj.org/article/120877104097420c83a19adbf17aef64
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
Jonathan E. Lambert, Braddock K. Linsley, Jordan T. Abell, Samantha C. Bova, Gisela Winckler, Yair Rosenthal, Thomas L. Weiss, Wei Huang
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 621:111578
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::22013e97e48579b5d35352917ecd5f77
https://doi.org/10.1016/j.palaeo.2023.111578
https://doi.org/10.1016/j.palaeo.2023.111578
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
Cheng Zeng, Shital P. Godad, Mi Yan, Zhengyu Liu, S. C. Bova, Anthony J. Broccoli, Yair Rosenthal
Publikováno v:
Nature. 600:E4-E6
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2fcda473aa1a3160771d31c4b4d9a1fa
https://doi.org/10.1038/s41586-021-03931-3
https://doi.org/10.1038/s41586-021-03931-3
Publikováno v:
Nature. 589:548-553
Proxy reconstructions from marine sediment cores indicate peak temperatures in the first half of the last and current interglacial periods (the thermal maxima of the Holocene epoch, 10,000 to 6,000 years ago, and the last interglacial period, 128,000
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f4fc2f8c97592502f70caf440343b68f
https://doi.org/10.1038/s41586-020-03155-x
https://doi.org/10.1038/s41586-020-03155-x