Eastern equatorial Pacific cold tongue during the Last Glacial Maximum as seen from alkenone paleothermometry
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- Type
- article
- Published
- 2009-12-01
- Cited by
- 57
- References
- 66
- Access
- Open access
- OpenAlex
- https://openalex.org/W1582736910
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:128634821
Keywords
Alkenone, Geology, Last Glacial Maximum, Oceanography, Foraminifera
References
- World ocean atlas
- Seasonal reconstructions of the earth's surface at the last glacial maximum
- Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes
- A 70‐kyr sea surface temperature record off southern Chile (Ocean Drilling Program Site 1233)
- Influence of volcanic shards on foraminiferal Mg/Ca in a core from the Galápagos region
- The upper end of the UK′37 temperature calibration revisited
- Eastern tropical Pacific hydrologic changes during the past 27,000 years from D/H ratios in alkenones
- Northern timing of deglaciation in the eastern equatorial Pacific from alkenone paleothermometry
- Planktonic foraminifera, sea surface temperatures, and mechanisms of oceanic change in the Peru and south equatorial currents, 0–150 ka BP
- Multispecies approach to reconstructing eastern equatorial Pacific thermocline hydrography during the past 360 kyr
- Physiological impacts on alkenone paleothermometry
- La Niña-like conditions in the eastern equatorial Pacific and a stronger Choco jet in the northern Andes during the last glaciation
- A Role for the Tropical Pacific
- Precision of the current methods to measure the alkenone proxy U37K′ and absolute alkenone abundance in sediments: Results of an interlaboratory comparison study
- Glacial‐interglacial dynamics of the eastern equatorial Pacific cold tongue‐Intertropical Convergence Zone system reconstructed from oxygen isotope records
- El Niño–Southern Oscillation–like variability during glacial terminations and interlatitudinal teleconnections
- Thorium‐230 normalized particle flux and sediment focusing in the Panama Basin region during the last 30,000 years
- An Estimate of Equatorial Upwelling in the Pacific
- Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations
- Systematic change of foraminiferal Mg/Ca ratios across a strong salinity gradient
Cited by
- Hydrological evolution of the eastern tropical Pacific during the last 430,000 years [an abstract of dissertation and a summary of dissertation review]
- Late quaternary sea bottom conditions in the southern Panama basin, Eastern Equatorial Pacific
- Alkenone unsaturation in surface sediments from the eastern equatorial Pacific: Implications for SST reconstructions
- Spatial reorganization in the equatorial divergence in the Eastern Tropical Pacific during the last 150 kyr
- El Niño–Southern Oscillation extrema in the Holocene and Last Glacial Maximum
- Assessing the impact of Laurentide Ice Sheet topography on glacial climate
- Nutricline shoaling in the eastern Pacific warm pool during the last two glacial maxima
- Progressive glacial retreat in the Southern Altiplano (Uturuncu volcano, 22°S) between 65 and 14 ka constrained by cosmogenic 3He dating
- Shoaling of the western equatorial Pacific thermocline during the last glacial maximum inferred from multispecies temperature reconstruction of planktonic foraminifera
- 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
- Influences of extratropical water masses on equatorial Pacific cold tongue variability during the past 160 ka as revealed by faunal evidence of planktic foraminifers
- Boron isotope evidence for oceanic carbon dioxide leakage during the last deglaciation
- Precession forcing of productivity in the Eastern Equatorial Pacific during the last glacial cycle
- Deglacial dust provenance changes in the Eastern Equatorial Pacific and implications for ITCZ movement
- Western Pacific thermocline structure and the Pacific marine Intertropical Convergence Zone during the Last Glacial Maximum
- Geochemical and climate modeling evidence for Holocene aridification in Hawaii: dynamic response to a weakening equatorial cold tongue
- Glacial cooling as inferred from marine temperature proxies TEX H 86 and U K′ 37
- Millennial-scale Atlantic/East Pacific sea surface temperature linkages during the last 100,000 years
- Millennial-scale variations in hydrography and biogeochemistry in the Eastern Equatorial Pacific over the last 100 kyr
- Comment on “A 12-million-year temperature history of the tropical Pacific Ocean”
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