Eastern North Atlantic deep-sea corals: tracing upper intermediate water Δ14C during the Holocene
- 11 February 2004
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 219 (3-4) , 297-309
- https://doi.org/10.1016/s0012-821x(03)00721-0
Abstract
No abstract availableKeywords
This publication has 52 references indexed in Scilit:
- The North Atlantic atmosphere-sea surface 14C gradient during the Younger Dryas climatic eventPublished by Elsevier ,2002
- Global distribution of centennial-scale records for Marine Isotope Stage (MIS) 3: a databaseQuaternary Science Reviews, 2002
- A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, ChinaScience, 2001
- Further Application of Bomb 14C as a Tracer in the Atmosphere and OceanRadiocarbon, 1996
- Changes in Atmospheric Circulation and Ocean Ice Cover over the North Atlantic During the Last 41,000 YearsScience, 1994
- Evidence for general instability of past climate from a 250-kyr ice-core recordNature, 1993
- AMS 14C Study of Transient Events and of the Ventilation Rate of the Pacific Intermediate Water During the Last DeglaciationRadiocarbon, 1989
- Radiocarbon age of last glacial Pacific deep waterNature, 1988
- Radiocarbon measurements on coexisting benthic and planktic foraminifera shells: potential for reconstructing ocean ventilation times over the past 20 000 yearsNuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 1984
- Geosecs North Atlantic radiocarbon and tritium resultsEarth and Planetary Science Letters, 1974