Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Akitoshi Omori"'
Autor:
Kazuhiko Fujita, Akitoshi Omori
Publikováno v:
Island Arc. 24:47-60
This paper reports the fauna and distribution of large-sized benthic foraminifers (LsBFs; defined as benthic foraminifers >0.5 mm in size) from surface sediments collected around Tahiti, French Polynesia, as well as from the Pleistocene deposits dril
Autor:
Yasunari Takahashi, Nicolas Durand, Terry Quinn, Alexander L. Thomas, Gilbert Camoin, Edouard Bard, Andrew J. Mason, Katrin Heindel, Akitoshi Omori, Hiroki Matsuda, Tokiyuki Sato, Saburo Sakai, Lucie Menabreaz, Alexander W. Tudhope, Kazuhiko Fujita, Yusuke Yokoyama, Bruno Hamelin, Jody M. Webster, Hildegard Westphal, Pierre Deschamps, Guy Cabioch, Julia E. Cole, Kaoru Sugihara, Yasufumi Iryu, Nicolas Thouveny, Gideon M. Henderson
Publikováno v:
Marine Geology
Marine Geology, Elsevier, 2012, 295-298, pp.86-94. ⟨10.1016/j.margeo.2011.12.006⟩
Marine Geology, 2012, 295-298, pp.86-94. ⟨10.1016/j.margeo.2011.12.006⟩
Marine Geology, Elsevier, 2012, 295-298, pp.86-94. ⟨10.1016/j.margeo.2011.12.006⟩
Marine Geology, 2012, 295-298, pp.86-94. ⟨10.1016/j.margeo.2011.12.006⟩
International audience; We present uranium–thorium chronology for a 102 m core through a Pleistocene reef at Tahiti (French Polynesia) sampled during IODP Expedition 310 “Tahiti Sea Level”. We employ total and partial dissolution procedures on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d846aa8dd6a81bb9a81d33e8283e37c7
https://ora.ox.ac.uk/objects/uuid:b059b59d-5e83-4708-9c54-547dded52591
https://ora.ox.ac.uk/objects/uuid:b059b59d-5e83-4708-9c54-547dded52591
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 292(3-4):443-452
Coral reef cavities, crevasses, and caves are inhabited by cryptic communities. The sediments within the submarine Daidokutsu Cave (29 m water depth) on the fore-reef slope of Ie Island, Okinawa, Japan, preserve a fossil record of cryptic bivalve spe
Publikováno v:
Marine Geology. 271:149-155
The course of sea-level fluctuations during Termination II (TII; the penultimate deglaciation), which is critical for understanding ice-sheet dynamics and suborbital climate variability, has yet to be established. This is partly because most shallow-