Causes of high diatom productivity in Neogene Lake of the Southern Primorye
Author:
Affiliation:
1. FSC of the East Asia Terrestrial Biodiversity FEB RAS, Vladivostok, Russia
2. Far East Geological Institute, FEB RAS, Vladivostok, Russia
Abstract
Publisher
Farwater LLC
Reference13 articles.
1. Evzerov V.YA. Formirovanie mestorozhdenij diatomita na krajnem Severo-Zapade Rossii [Formation of diatomite deposits in the far North-West of Russia]. Vestnik Voronezhskogo Gosudarstvennogo Universiteta. Seriya: geologiya. 2011. № 2. P. 55–65. (In Russ.)
2. Flower B.P., Kennett J.P. Middle Miocene ocean-climate transition: High-resolution oxygen and carbon isotopic records from Deep Sea Drilling Project Site 588A, southwest Pacific. Paleoceanography. 1993. 8 (6). P. 811–843. DOI: https://doi.org/10.1029/93pa02196
3. Harry J.D., Chandler M.A., Cronin T.M., Dwyer G.S. Mid Pliocene Sea surface temperature variability. Paleoceanography. 2005. V.20, Is.2. PA2014. DOI: https://doi.org/10.1029/2005PA001133
4. Holbourn A., Kuhnt W., Schulz M., Flores J.A., Andersen N. Orbitally-paced climate evolution during the middle Miocene “Monterey” carbon-isotope excursion. Earth and Planetary Science Letters. 2007. V.261, №3–4. P. 534–550.
5. Jiang H., Ding Z.A. 20 Ma pollen record of East-Asian summer monsoon evolution from Guyuan, Ningxia, China. Palaeogeography, Palaeoclimatology, Palaeoecology. 2008. V.265. P. 30–38.
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