Planktonic foraminifera, calcareous nannoplankton and ascidian variations during the last 25 kyr in the Southwestern Atlantic: A paleoproductivity signature?
- 1 June 2007
- journal article
- Published by Elsevier in Marine Micropaleontology
- Vol. 64 (1-2) , 67-79
Abstract
No abstract availableKeywords
This publication has 45 references indexed in Scilit:
- Coccolith distribution patterns in South Atlantic and Southern Ocean surface sediments in relation to environmental gradientsDeep Sea Research Part I: Oceanographic Research Papers, 2006
- Late Pleistocene–Holocene paleoclimate and related paleoenvironmental changes as recorded by calcareous nannofossils and planktonic foraminifera assemblages in the southern Tyrrhenian Sea (Cape Palinuro, Italy)Marine Micropaleontology, 2004
- Distribution of coccoliths in surface sediments of the south-eastern South Atlantic Ocean: ecology, preservation and carbonate contributionMarine Micropaleontology, 2004
- Paleoceanographic implications of the difference in deep‐sea sediment mixing between large and fine particlesPaleoceanography and Paleoclimatology, 2001
- The deglacial history of the western tropical Atlantic as inferred from high resolution stable isotope records off northeastern BrazilEarth and Planetary Science Letters, 1999
- Calcitic foraminiferal data confirmed by cadmium in aragonitic Hoeglundina: Application to the Last Glacial Maximum in the northern Indian OceanPaleoceanography and Paleoclimatology, 1995
- Cadmium: Chemical tracer of deepwater paleoceanographyPaleoceanography and Paleoclimatology, 1988
- Where Are All the Fossil Sea Squirts?Micropaleontology, 1988
- North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperatureNature, 1987
- Standing stock, vertical distribution and flux of planktonic foraminifera in the Panama BasinMarine Micropaleontology, 1985