Mediterranean Sea surface radiocarbon reservoir age changes since the last glacial maximum.
Sea surface reservoir ages must be known to establish a common chronological framework for marine, continental, and cryospheric paleoproxies, and are crucial for understanding ocean-continent climatic relationships and the paleoventilation of the ocean. Radiocarbon dates of planktonic foraminifera and tephra contemporaneously deposited over Mediterranean marine and terrestrial regions reveal that the reservoir ages were similar to the modern one (approximately 400 years) during most of the past 18,000 carbon-14 years. However, reservoir ages increased by a factor of 2 at the beginning of the last deglaciation. This is attributed to changes of the North Atlantic thermohaline circulation during the massive ice discharge event Heinrich 1.
Siani
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G
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), Unité Mixte de Service, CNRS, Avenue de la Terrasse, F-91118 Gif-sur-Yvette, France.
Paterne
M
M
Michel
E
E
Sulpizio
R
R
Sbrana
A
A
Arnold
M
M
Haddad
G
G
D000818:Animals; D001267:Atlantic Ocean; D001272:Atmosphere; D002138:Calibration; D002244:Carbon / Q000378:metabolism; D002245:Carbon Dioxide / Q000378:metabolism; D002250:Carbon Radioisotopes / Q000378:metabolism; D003081:Cold Climate; D005618:Fresh Water; D019015:Geologic Sediments / Q000469:parasitology; D006116:Greenland; D007053:Ice; D008522:Mediterranean Sea; D010933:Plankton / Q000378:metabolism*; D012623:Seawater; D013696:Temperature; D013997:Time Factors; D018707:Volcanic Eruptions
D002250:Carbon Radioisotopes; D007053:Ice; D002245:Carbon Dioxide; D002244:Carbon