Diatom D18O evidence for the development of the modern halocline system in the subarctic northwest Pacific at the onset of major Northern Hemisphere glaciationTools Swann, George E.A., Maslin, Mark A., Leng, Melanie J., Sloane, Hilary J. and Haug, Gerald H. (2006) Diatom D18O evidence for the development of the modern halocline system in the subarctic northwest Pacific at the onset of major Northern Hemisphere glaciation. Paleoceanography, 21 (PA1009). ISSN 1944-9186 Full text not available from this repository.
Official URL: http://dx.doi.org/10.1029/2005PA001147
AbstractEstablishing a time frame for the development of the modern halocline and stratified water column in the subarctic North Pacific has significant paleoclimatic implications. Here we present a d18O(diatom) record consisting of only two species that represents autumn/winter conditions in the region across the onset of major Northern Hemisphere glaciation boundary. At circa 2.73 Ma a decrease in d18O(diatom) of 4.6% occurs, whereas previously published d18O(foram) results show a 2.6% increase. The d18O(diatom) and Uk37 sea surface reconstructions indicate both a significant freshening of 2–4 practical salinity units and an increase in surface temperatures in the summer to early winter period from circa 2.73 Ma onward. In contrast, the concomitant increase in d18O(foram) is likely to be reflective of conditions beneath the mesothermal structure and/or spring
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