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(Table A8) Sedimentology of ODP Hole 154-926A

Publication Date
DOI: 10.1594/pangaea.67500
  • 154-926A
  • Accumulation Rate
  • Calcium Carbonate
  • Accumulation Rate
  • Sand > 63 µM
  • Accumulation Rate
  • Siliciclastics
  • Calculated
  • See Reference(S)
  • Carbonates
  • Drilling
  • Element Analyser Chn
  • Leco
  • Geomar
  • Grain Size
  • Sieving
  • Helmholtz Centre For Ocean Research Kiel
  • Joides Resolution
  • Leg154
  • North Atlantic Ocean
  • Ocean Drilling Program
  • Odp
  • Odp Sample Designation
  • Sample Code/Label
  • Sand
  • Sedimentation Rate
  • Siliciclastics
  • Size Fraction > 0
  • 063 Mm
  • Sand


pa001868 1..15 Click Here for Full Article More humid interglacials in Ecuador during the past 500 kyr linked to latitudinal shifts of the equatorial front and the Intertropical Convergence Zone in the eastern tropical Pacific Daniel Rincón‐Martínez,1 Frank Lamy,1 Sergio Contreras,2 Guillaume Leduc,3 Edouard Bard,4 Cornelia Saukel,1 Thomas Blanz,3 Andreas Mackensen,1 and Ralf Tiedemann1 Received 8 October 2009; revised 10 February 2010; accepted 24 March 2010; published 2 June 2010. [1] Studying past changes in the eastern equatorial Pacific Ocean dynamics and their impact on precipitation on land gives us insight into how the Intertropical Convergence Zone (ITCZ) movements and the El Niño‐Southern Oscillation modulate regional and global climate. In this study we present a multiproxy record of terrigenous input from marine sediments collected off the Ecuadorian coast spanning the last 500 kyr. In parallel we estimate sea surface temperatures (SST) derived from alkenone paleothermometry for the sediments off the Ecuadorian coast and complement them with alkenone‐based SST data from the Panama Basin to the north in order to investigate SST gradients across the equatorial front. Near the equator, today’s river runoff is tightly linked to SST, reaching its maximum either during the austral summer when the ITCZ migrates southward or during El Niño events. Our multiproxy reconstruction of riverine runoff indicates that interglacial periods experienced more humid conditions than the glacial periods. The north‐south SST gradient is systematically steeper during glacial times, suggesting a mean background climatic state with a vigorous oceanic cold tongue, resembling modern La Niña conditions. This enhanced north‐south SST gradient would also imply a glacial northward shift of the Intertropical Convergence Zone at least in vicinity of the cold tongue: a pattern that has not yet been reproduced in climate models. Citation: Rincón‐Martínez, D., F. Lamy, S. Contreras, G. Leduc, E. Bard,

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