Zobrazeno 1 - 10
of 485
pro vyhledávání: '"R. Tada"'
Autor:
P. D. Clift, C. Betzler, S. C. Clemens, B. Christensen, G. P. Eberli, C. France-Lanord, S. Gallagher, A. Holbourn, W. Kuhnt, R. W. Murray, Y. Rosenthal, R. Tada, S. Wan
Publikováno v:
Scientific Drilling, Vol 31, Pp 1-29 (2022)
The International Ocean Discovery Program (IODP) conducted a series of expeditions between 2013 and 2016 that were designed to address the development of monsoon climate systems in Asia and Australia. Significant progress was made in recovering Neoge
Externí odkaz:
https://doaj.org/article/90bffdbbff91417fae28df302dfdbdbe
Publikováno v:
Scientific Drilling, Vol 24, Pp 87-91 (2018)
The IODP-PAGES Workshop on Global Monsoon in Long-term Records was held on 7–9 September 2017, in Shanghai, China. Forty-eight scientists from 12 countries exchanged scientific findings from the seven recent IODP monsoon-related expeditions (see
Externí odkaz:
https://doaj.org/article/32ae328545bc4a238cf4e1b336ae2ec5
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 19, Iss 8, Pp 2463-2477 (2018)
Abstract We examine the paleoceanographic record over the last ∼400 kyr derived from major, trace, and rare earth elements in bulk sediment from two sites in the East China Sea drilled during Integrated Ocean Drilling Program Expedition 346. We use
Externí odkaz:
https://doaj.org/article/98e3998ac4f4489aac29d75226e8e681
Publikováno v:
Climate of the Past, Vol 11, Iss 2, Pp 265-281 (2015)
The δ18O of seawater (δ18Ow), an indirect indicator of sea surface salinity (SSS), in the northern East China Sea (ECS) is reconstructed for the Holocene using paired analyses of Mg / Ca ratio and δ18O of planktic foraminiferal tests. According to
Externí odkaz:
https://doaj.org/article/98ff25a9fe1b49259889afd5d52fa7d6
Autor:
H. Hasegawa, R. Tada, X. Jiang, Y. Suganuma, S. Imsamut, P. Charusiri, N. Ichinnorov, Y. Khand
Publikováno v:
Climate of the Past, Vol 8, Iss 4, Pp 1323-1337 (2012)
Understanding the behavior of the global climate system during extremely warm periods is one of the major themes of paleoclimatology. Proxy data demonstrate that the equator-to-pole temperature gradient was much lower during the mid-Cretaceous "super
Externí odkaz:
https://doaj.org/article/720d9d0bb1114585a8f3005b8d7edaee
Autor:
W. Bach, C. Ravelo, J. Behrmann, G. Camoin, R. Duncan, K. Edwards, S. Gulick, F. Inagaki, H. Pälike, R. Tada
Publikováno v:
Scientific Drilling, Vol 9, Pp 54-64 (2010)
No abstract available. doi:10.2204/iodp.sd.9.12.2010
Externí odkaz:
https://doaj.org/article/4d80215ab654464ba893472215fed458
Autor:
J. Thurow, L. C. Peterson, U. Harms, D. A. Hodell, H. Cheshire, H.-J. Brumsack, T. Irino, M. Schulz, V. Masson-Delmotte, R. Tada
Publikováno v:
Scientific Drilling, Vol 8, Pp 46-56 (2009)
No abstract available. doi:10.2204/iodp.sd.8.08.2009
Externí odkaz:
https://doaj.org/article/e84e7c1902a74c4887f89565a8ba0996
Publikováno v:
Biogeosciences, Vol 5, Iss 3, Pp 797-816 (2008)
We determined both the nitrogen and carbon isotopic compositions of various vanadyl alkylporphyrins isolated from siliceous marine sediments of the Onnagawa Formation (middle Miocene, northeastern Japan) to investigate the biogeochemistry and ecology
Externí odkaz:
https://doaj.org/article/32ffcd779ea842cb8b59a6d82670c989
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Akademický článek
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