Younger Dryas‐Style Cooling Events at Glacial Terminations I‐VI at ODP Site 658: Associated benthic δ¹³C anomalies constrain meltwater hypothesis

This publication has 44 references indexed in Scilit:

• The cause of the glacial to interglacial atmospheric CO₂ change: A Polar Alkalinity Hypothesis
  Global Biogeochemical Cycles, 1989
• Pleistocene evolution: Northern hemisphere ice sheets and North Atlantic Ocean
  Paleoceanography and Paleoclimatology, 1989
• Comparison between radiocarbon ages obtained on coexisting planktonic foraminifera
  Paleoceanography and Paleoclimatology, 1988
• Global variations of surface ocean productivity in low and mid latitudes: Influence on CO₂ reservoirs of the deep ocean and atmosphere during the last 21,000 years
  Paleoceanography and Paleoclimatology, 1988
• The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas Event
  Paleoceanography and Paleoclimatology, 1988
• Reconstruction of the last deglaciation: deconvolved records of ?18O profiles, micropaleontological variations and accelerator mass spectrometric14C dating
  Climate Dynamics, 1987
• The impact of cold North Atlantic sea surface temperatures on climate: implications for the Younger Dryas cooling (11?10 k)
  Climate Dynamics, 1986
• Graphic correlation of oxygen isotope stratigraphy application to the Late Quaternary
  Paleoceanography and Paleoclimatology, 1986
• Benthic foraminiferal δ13C and accumulation rates of organic carbon: Uvigerina Peregrina group and Cibicidoides Wuellerstorfi
  Paleoceanography and Paleoclimatology, 1986
• Insolation changes, ice volumes, and the O¹⁸ record in deep‐sea cores
  Reviews of Geophysics, 1970