Silicon-isotope composition of diatoms as an indicator of past oceanic change
- 15 October 1998
- journal article
- Published by Springer Nature in Nature
- Vol. 395 (6703), 680-683
- https://doi.org/10.1038/27174
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Can the aluminum and titanium contents of ocean sediments be used to determine the paleoproductivity of the oceans?Paleoceanography and Paleoclimatology, 1997
- Increased biological productivity and export production in the glacial Southern OceanNature, 1995
- Production and dissolution of biogenic silica in the ocean: Revised global estimates, comparison with regional data and relationship to biogenic sedimentationGlobal Biogeochemical Cycles, 1995
- The Silica Balance in the World Ocean: A ReestimateScience, 1995
- Late Pleistocene oxygen isotope records of biogenic silica from the Atlantic sector of the Southern OceanPaleoceanography and Paleoclimatology, 1995
- Meltwater Input to the Southern Ocean During the Last Glacial MaximumScience, 1994
- River Fluxes of Dissolved Silica to the Ocean Were Higher during Glacials: Ge/Si In Diatoms, Rivers, and OceansPaleoceanography and Paleoclimatology, 1992
- Biogenic opal in Southern Ocean sediments over the last 450,000 years: Implications for surface water chemistry and circulationPaleoceanography and Paleoclimatology, 1991
- Primary productivity and the silica cycle in the Southern Ocean (Atlantic sector)Palaeogeography, Palaeoclimatology, Palaeoecology, 1988
- Origin of Diatom Ooze Belt in the Southern Ocean: Implications for Late Quaternary PaleoceanographyMicropaleontology, 1987