Articles | Volume 8, issue 1
https://doi.org/10.5194/cp-8-17-2012
© Author(s) 2012. This work is distributed under the Creative Commons Attribution 3.0 License.
Research article
| 
03 Jan 2012
Research article |
| 03 Jan 2012
Ventilation changes in the western North Pacific since the last glacial period
Related subject area
Subject: Carbon Cycle | Archive: Marine Archives | Timescale: Millenial/D-O
Deglacial carbon cycle changes observed in a compilation of 127 benthic δ13C time series (20–6 ka)
δ13C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2
Peak glacial 14C ventilation ages suggest major draw-down of carbon into the abyssal ocean
Marine productivity response to Heinrich events: a model-data comparison
Clim. Past, 14, 1229–1252, 2018
Clim. Past, 13, 345–358, 2017
Clim. Past, 9, 2595–2614, 2013
Clim. Past, 8, 1581–1598, 2012
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Ahagon, N., Ohkushi, K., Uchida, M., and Mishima, T.: Mid-depth circulation in the northwest Pacific during the last deglaciation: Evidence from foraminiferal radiocarbon ages, Geophys. Res. Lett., 30, 2097, https://doi.org/10.1029/2003GL018287, 2003.
Bevington, P. R. and Robinson, K. D.: Data reduction and error analysis for the physical sciences, third edition, McGraw-Hill, New York, 2003.
Broecker, W. and Barker, S.: A 190 \permil drop in atmosphere's Δ14C during the "Mystery Interval" (17.5 to 14.5 kyr), Earth Planet. Sci. Lett., 256, 90–99, 2007.
Broecker, W., Mix, A., Andree, M., and Oeschger, H.: Radiocarbon measurements on coexisting benthic and planktic foraminifera shells: potential for reconstructing ocean ventilation times over the past 20000 years, Nucl. Instr. Meth., B, 5, 331–339, 1984.
