Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/98306
Title: Impact of suborbital climate changes in the North Atlantic on ice sheet dynamics at the Mid-Pleistocene Transition
Author: Hernandez-Almeida, I.
Sierro Sánchez, Francisco Javier
Cacho Lascorz, Isabel
Flores Villarejo, José Abel
Keywords: Paleoceanografia
Paleoclimatologia
Plistocè
Atlàntic, Oceà
Paleoceanography
Paleoclimatology
Pleistocene
Atlantic Ocean
Issue Date: 16-Aug-2012
Publisher: American Geophysical Union
Abstract: Early and Mid-Pleistocene climate, ocean hydrography and ice sheet dynamics have been reconstructed using a high-resolution data set (planktonic and benthic delta O-18 time series, faunal-based sea surface temperature (SST) reconstructions and ice-rafted debris (IRD)) record from a high-deposition-rate sedimentary succession recovered at the Gardar Drift formation in the subpolar North Atlantic (Integrated Ocean Drilling Program Leg 306, Site U1314). Our sedimentary record spans from late in Marine Isotope Stage (MIS) 31 to MIS 19 (1069-779 ka). Different trends of the benthic and planktonic oxygen isotopes, SST and IRD records before and after MIS 25 (similar to 940 ka) evidence the large increase in Northern Hemisphere ice-volume, linked to the cyclicity change from the 41-kyr to the 100-kyr that occurred during the Mid-Pleistocene Transition (MPT). Beside longer glacial-interglacial (G-IG) variability, millennial-scale fluctuations were a pervasive feature across our study. Negative excursions in the benthic delta O-18 time series observed at the times of IRD events may be related to glacio-eustatic changes due to ice sheets retreats and/or to changes in deep hydrography. Time series analysis on surface water proxies (IRD, SST and planktonic delta O-18) of the interval between MIS 31 to MIS 26 shows that the timing of these millennial-scale climate changes are related to half-precessional (10 kyr) components of the insolation forcing, which are interpreted as cross-equatorial heat transport toward high latitudes during both equinox insolation maxima at the equator.
Note: Reproducció del document publicat a: http://dx.doi.org/10.1029/2011PA002209
It is part of: Paleoceanography, 2012, vol. 27, num. 3, p. 1-14
Related resource: http://dx.doi.org/10.1029/2011PA002209
URI: http://hdl.handle.net/2445/98306
ISSN: 0883-8305
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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