Changes of marine productivity and sedimentary environment recorded by biogenic components in the Antarctica Ross Sea since the last deglaciation
Author:
Publisher
Springer Science and Business Media LLC
Subject
Water Science and Technology,Oceanography
Link
http://link.springer.com/content/pdf/10.1007/s00343-019-9218-2.pdf
Reference44 articles.
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2. Barnola J M, Raynaud D, Korotkevich Y S, Lorius C. 1987. Vostok ice core provides 160,000-year record of atmospheric CO2. Nature, 329(6138): 408–414, https://doi.org/10.1038/329408a0.
3. Bathmann U V, Scharek R, Klaas C, Dubischar C D, Smetacek V. 1997. Spring development of phytoplankton biomass and composition in major water masses of the Atlantic sector of the Southern Ocean. Deep Sea Research Part II:. Topical Studies in Oceanography, 44(1–2): 51–67, https://doi.org/10.1016/S0967-0645(96)00063-X.
4. Bentaleb I, Fontugne M. 1998. The role of the southern Indian Ocean in the glacial to interglacial atmospheric CO2 change: organic carbon isotope evidences. Global and Planetary Change, 16–17: 25–36, https://doi.org/10.1016/S0921-8181(98)00004-6.
5. Bonn W J, Gingele F X, Grobe H, Mackensen A, Fütterer D K. 1998. Palaeoproductivity at the Antarctic continental margin: opal and barium records for the last 400 ka. Palaeogeography, Palaeoclimatology, Palaeoecology, 139(3–4): 195–211, https://doi.org/10.1016/S0031-0182(97)00144-2.
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