Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial.

@article{Peterson2000RapidCI,
  title={Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial.},
  author={Larry C. Peterson and Gerald H. Haug and Konrad A. Hughen and Ursula R{\"o}hl},
  journal={Science},
  year={2000},
  volume={290 5498},
  pages={
          1947-51
        }
}
Sedimentary time series of color reflectance and major element chemistry from the anoxic Cariaco Basin off the coast of northern Venezuela record large and abrupt shifts in the hydrologic cycle of the tropical Atlantic during the past 90,000 years. Marine productivity maxima and increased precipitation and riverine discharge from northern South America are closely linked to interstadial (warm) climate events of marine isotope stage 3, as recorded in Greenland ice cores. Increased precipitation… 
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References

SHOWING 1-10 OF 24 REFERENCES
Rapid climate changes in the tropical Atlantic region during the last deglaciation
THE climate system is capable of changing abruptly from one stable mode to another1–3. Rapid climate oscillations—in particular the Younger Dryas cold period during the last deglaciation—have long
Eight centuries of north atlantic ocean atmosphere variability
TLDR
A high-resolution study of Caribbean sediments provides a subdecadally resolved record of tropical upwelling and trade wind variability spanning the past 825 years, confirming the importance of a decadal mode of Atlantic variability believed to be driven by coupled tropical ocean-atmosphere dynamics.
Pleistocene Precipitation Balance in the Amazon Basin Recorded in Deep Sea Sediments
Abstract Terrigenous sediments from Ceara Rise in the western tropical Atlantic Ocean record Pleistocene Amazon Basin climate variability. Iron oxides and oxyhydroxides in this region originate
Correlated Millennial-Scale Changes in Surface Hydrography and Terrigenous Sediment Yield Inferred from Last-Glacial Marine Deposits off Northeastern Brazil
The stable isotope composition of planktonic foraminifera correlates with evidence for pulses of terrigenous sediment in a sediment core from the upper continental slope off northeastern Brazil.
A high-resolution late Quaternary upwelling record from the anoxic Cariaco Basin, Venezuela
Results are presented of a high-resolution study of the planktonic foraminiferal faunas from two piston cores recovered from the Cariaco Basin in the southern Caribbean Sea. The Cariaco Basin is a
Correlations between climate records from North Atlantic sediments and Greenland ice
OXYGEN isotope measurements in Greenland ice demonstrate that a series of rapid warm-cold oscillations—called Dansgaard–Oeschger events—punctuated the last glaciation1. Here we present records of sea
Brief interstadial events in the Santa Barbara basin, NE Pacific, during the past 60 kyr
THE instability of the Northern Hemisphere glacial climate over the past 100 kyr has been revealed by at least 20 brief warm (interstadial) episodes, called Dansgaard–Oeschger events, recorded in
Late Quaternary climate change from δ18O records of multiple species of planktonic foraminifera: High‐resolution records from the Anoxic Cariaco Basin, Venezuela
Seasonal trade wind-induced upwelling along the southern margin of the Caribbean Sea occurs in response to the annual migration of the Intertropical Convergence Zone. Laminated, high deposition rate
Mountain glaciers: Recorders of atmospheric water vapor content?
A case is made that taken together, the 0.9 km lowering of tropical snow lines and the 8‰ reduction in the δ18O for tropical mountain Huascarán snowfall point to reductions in the water vapor
Tropical Cooling at the Last Glacial Maximum: An Atmosphere-Mixed Layer Ocean Model Simulation
The sensitivity of tropical temperature to glacial forcing is examined by using an atmosphere‐mixed layer ocean (A‐MLO) model to simulate the climate of the last glacial maximum (LGM) following
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