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El Niño/Southern Oscillation and tropical Pacific climate during the last millennium

Fossil-coral oxygen isotopic records from Palmyra Island are splice together to provide 30–150-year windows of tropical Pacific climate variability within the last 1,100 years, implying that the majority of ENSO variability over the last millennium may have arisen from dynamics internal to the ENSo system itself.
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The oxygen isotopic composition of seawater during the Last Glacial Maximum

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Changes in the mode of Southern Ocean circulation over the last glacial cycle revealed by foraminiferal stable isotopic variability

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Origin of Global Meltwater Pulses

The fact that frequencies measured in climate records are the same as those predicted by the astronomical theory of climate change is undisputed (Hays, Imbrie & Shackleton 1976). However, the…
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Pleistocene vertical carbon isotope and carbonate gradients in the South Atlantic sector of the Southern Ocean

We demonstrate that the carbon isotopic signal of mid‐depth waters evolved differently from deep waters in the South Atlantic sector of the Southern Ocean during the Pleistocene. Deep sites (>3700 m)…
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Abrupt Cooling of Antarctic Surface Waters and Sea Ice Expansion in the South Atlantic Sector of the Southern Ocean at 5000 cal yr B.P.

Abstract Antarctic surface waters were warm and ice free between 10,000 and 5000 cal yr B.P., as judged from ice-rafted debris and microfossils in a piston core at 53°S in the South Atlantic. This…
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Interaction Between the ENSO and the Asian Monsoon in a Coral Record of Tropical Climate

The oxygen isotopic composition of a banded coral from the western equatorial Indian Ocean provides a 150-year-long history of the relation between the El Nino–Southern Oscillation (ENSO) phenomenon…
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Evaluating climate indices and their geochemical proxies measured in corals

Abstract. Standard ocean/climate indices such as the Niño-3 sea surface temperature (SST) index, based on sparse instrumental data, and atmospheric indices such as the Southern Oscillation Index…
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Climate connections between the hemisphere revealed by deep sea sediment core/ice core correlations

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Evidence from Southern Ocean sediments for the effect of North Atlantic deep-water flux on climate

The Southern Ocean is perhaps the only region where fluctuations in the global influence of North Atlantic Deep Water (NADW) can be monitored unambiguously in single deep-sea cores. A carbon isotope…
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