Zobrazeno 1 - 6
of 6
pro vyhledávání: '"R. M. Leckie"'
Publikováno v:
Journal of Micropalaeontology, Vol 43, Pp 383-421 (2024)
The Ross Sea record of the Miocene Climatic Optimum (MCO; ∼ 16.9–14.7 Ma) and the Middle Miocene Climate Transition (MMCT; ∼ 14.7–13.8 Ma) provides critical insights into Antarctic ocean–cryosphere interactions during a time of extreme warm
Externí odkaz:
https://doaj.org/article/335fdb565c614db6a7b26794f09109ef
Publikováno v:
Journal of Micropalaeontology, Vol 43, Pp 211-238 (2024)
International Ocean Discovery Program (IODP) Expedition 374 sailed to the Ross Sea in 2018 to reconstruct paleoenvironments, track the history of key water masses, and assess model simulations that show warm-water incursions from the Southern Ocean l
Externí odkaz:
https://doaj.org/article/e58a7b3ec99444309331d9ae61374feb
Publikováno v:
Journal of Micropalaeontology, Vol 43, Pp 187-209 (2024)
In 1977–1978 and 1978–1979, the Ross Ice Shelf Project (RISP) recovered sediments from beneath the largest ice shelf in Antarctica at Site J-9 (∼82° S, 168° W), ∼450 km from open marine waters at the calving front of the Ross Ice Shelf and
Externí odkaz:
https://doaj.org/article/68c55481b1484b46a1b28ceb48cde795
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
R. M. Leckie, Simon P. Kelley, John W. King, Haraldur Sigurdsson, Steven Carey, Timothy J Bralower
Drilling in the Caribbean Sea during Ocean Drilling Program Leg 165 has recovered a large number of silicic tephra layers and led to the discovery of three major episodes of explosive volcanism that occurred during the last 55 m.y. on the margins of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b98f9d3aa14056ec99e1f345bf3151de
https://doi.org/10.2973/odp.proc.sr.165.021.2000
https://doi.org/10.2973/odp.proc.sr.165.021.2000
Publikováno v:
Geological Society of America Bulletin. 109:1421
Large variations exist between published mid-Cretaceous (late Barremian to early Turonian stages) seawater Sr-isotope stratigraphies; this has resulted in disparate interpretations of crustal production rates. We report on a detailed investigation of