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Title

Sediment instability on the Portuguese continental margin under abrupt glacial climate changes (last 60 kyr)

AuthorsLebreiro, S. M.; Voelker, A. H. L.; Vizcaino, A. ; Abrantes, Fátima; Alt-Epping, U.; Jung, S.; Thouveny, N.; Gràcia, Eulàlia
Issue DateDec-2009
PublisherElsevier
CitationQuaternary Science Reviews 28(27-28): 3211-3223 (2009)
AbstractIt is well established that orbital scale sea-level changes generated larger transport of sediments into the deep-sea during the last glacial maximum than the Holocene. However, the response of sedimentary processes to abrupt millennial-scale climate variability is rather unknown. Frequency of distal turbidites and amounts of advected detrital carbonate are estimated off the Lisbon-Setúbal canyons (core MD03-2698, at 4602 mwd), within a chronostratigraphy based on radiometric ages, oxygen isotopes and paleomagnetic key global anomalies. We found that: 1) higher frequency of turbidites concurred with Northern Hemisphere coldest temperatures (Greenland Stadials [GS], including Heinrich [H] events). But more than that, an escalating frequency of turbidites starts with the onset of global sea-level rising (and warming in Antarctica) and culminates during H events, at the time when rising is still in its early-mid stage, and the Atlantic Meridional Overturning Circulation (AMOC) is re-starting. This short time span coincides with maximum gradients of ocean surface and bottom temperatures between GS and Antarctic warmings (Antarctic Isotope Maximum; AIM 17, 14, 12, 8, 4, 2) and rapid sea-level rises. 2) Trigger of turbidity currents is not the only sedimentary process responding to millennial variability; land-detrital carbonate (with a very negative bulk δ18O signature) enters the deep-sea by density-driven slope lateral advection, accordingly during GS. 3) Possible mechanisms to create slope instability on the Portuguese continental margin are sea-level variations as small as 20 m, and slope friction by rapid deep and intermediate re-accommodation of water masses circulation. 4) Common forcing mechanisms appear to drive slope instability at both millennial and orbital scales. © 2009
Description13 pages, 6 figures, 1 table, appendix supplementary information
Publisher version (URL)http://dx.doi.org/10.1016/j.quascirev.2009.08.007
URIhttp://hdl.handle.net/10261/101067
DOI10.1016/j.quascirev.2009.08.007
Identifiersdoi: 10.1016/j.quascirev.2009.08.007
issn: 0277-3791
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