Metastable CaCO3dissolution at intermediate water depths of the Caribbean and western North Atlantic: Implications for intermediate water circulation during the past 200,000 years
- 1 December 1996
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 11 (6) , 701-716
- https://doi.org/10.1029/96pa02406
Abstract
No abstract availableKeywords
This publication has 55 references indexed in Scilit:
- Quaternary paleo-oceanography, pteropod preservation and stable-isotope record of the Red SeaPalaeogeography, Palaeoclimatology, Palaeoecology, 1986
- Banktop responses to Quaternary fluctuations in sea level recorded in periplatform sedimentsGeology, 1986
- Sources of Periplatform Carbonates: Northwest Providence Channel, BahamasJournal of Sedimentary Research, 1984
- Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical EvidenceScience, 1982
- Deep-sea carbonate: pteropod distribution and the aragonite compensation depthDeep Sea Research, 1978
- Deep-sea carbonate and the deglaciation preservation spike in pteropods and foraminiferaNature, 1977
- Sedimentation and Dissolution of Pteropods in the OceanPublished by Springer Nature ,1977
- Aragonite dissolution on the Bermuda pedestal: Its depth and geochemical significanceEarth and Planetary Science Letters, 1976
- Deep-sea carbonates; Pleistocene dissolution cyclesJournal of Foraminiferal Research, 1973
- Planktonic Foraminifera: selective solution and paleoclimatic interpretationDeep Sea Research and Oceanographic Abstracts, 1968