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@article{Deaney:2017:10.1038/ncomms14595,
author = {Deaney, EL and Barker, S and van, de Flierdt T},
doi = {10.1038/ncomms14595},
journal = {Nature Communications},
title = {Timing and nature of AMOC recovery across Termination 2 and magnitude of deglacial CO2 change},
url = {http://dx.doi.org/10.1038/ncomms14595},
volume = {8},
year = {2017}
}

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TY  - JOUR
AB - Large amplitude variations in atmospheric CO2were associated with glacial terminationsof the Late Pleistocene. Here we provide multiple lines of evidence suggesting that theB20 p.p.m.v. overshoot in CO2at the end of Termination 2 (T2)B129 ka was associated withan abrupt (r400 year) deepening of Atlantic Meridional Overturning Circulation (AMOC).In contrast to Termination 1 (T1), which was interrupted by the Bølling-Allerød (B-A), AMOCrecovery did not occur until the very end of T2, and was characterized by pronouncedformation of deep waters in the NW Atlantic. Considering the variable influences of oceancirculation change on atmospheric CO2, we suggest that the net change in CO2across thelast 2 terminations was approximately equal if the transient effects of deglacial oscillations inocean circulation are taken into account.
AU - Deaney,EL
AU - Barker,S
AU - van,de Flierdt T
DO - 10.1038/ncomms14595
PY - 2017///
SN - 2041-1723
TI - Timing and nature of AMOC recovery across Termination 2 and magnitude of deglacial CO2 change
T2 - Nature Communications
UR - http://dx.doi.org/10.1038/ncomms14595
UR - http://hdl.handle.net/10044/1/44100
VL - 8
ER -