Zobrazeno 1 - 4
of 4
pro vyhledávání: '"K. W. R. Taylor"'
Autor:
C. J. Hollis, S. Naeher, C. D. Clowes, B. D. A. Naafs, R. D. Pancost, K. W. R. Taylor, J. Dahl, X. Li, G. T. Ventura, R. Sykes
Publikováno v:
Climate of the Past, Vol 18, Pp 1295-1320 (2022)
Late Paleocene deposition of an organic-rich sedimentary facies on the continental shelf and slope of New Zealand and eastern Australia has been linked to short-lived climatic cooling and terrestrial denudation following sea leve
Externí odkaz:
https://doaj.org/article/f3e4419e18354e1b910b1f0a1402743f
Autor:
K. Schmidt, T. A. Brown, S. T. Belt, L. C. Ireland, K. W. R. Taylor, S. E. Thorpe, P. Ward, A. Atkinson
Publikováno v:
Biogeosciences, Vol 15, Pp 1987-2006 (2018)
Sea ice affects primary production in polar regions in multiple ways. It can dampen water column productivity by reducing light or nutrient supply, provide a habitat for ice algae and condition the marginal ice zone (MIZ) for phytoplankton blooms
Externí odkaz:
https://doaj.org/article/3d76c52eb57a40c9a57a8e66dddc0736
Autor:
S. T. Belt, L. Smik, T. A. Brown, J.-H. Kim, S. J. Rowland, C. S. Allen, J.-K. Gal, K.-H. Shin, J. I. Lee, K. W. R. Taylor
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-10 (2016)
The sedimentary presence of the diatom lipid diene II (hereafter IPSO25) has been proposed as a proxy for palaeo Antarctic sea ice. Here, the authors identify a source of IPSO25and hypothesize that its sedimentary distribution may provide proxy evide
Externí odkaz:
https://doaj.org/article/9a72d7cb3b6341f58cab6edb8b26e756
Publikováno v:
29th International Meeting on Organic Geochemistry.