No‐analog communities (communities that are compositionally unlike any found today)
occurred frequently in the past and will develop in the greenhouse world of the future. The …

Oceans cover more than two-thirds of our blue planet. The waters move in a global
circulation system, driven by subtle density differences and transporting huge amounts of …

Deciphering the evolution of global climate from the end of the Last Glacial Maximum
approximately 19 ka to the early Holocene 11 ka presents an outstanding opportunity for …

Abstract The variability of El Niño/Southern Oscillation (ENSO) during the Holocene epoch,
in particular on millennial timescales, is poorly understood. Palaeoclimate studies have …

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 …

Abrupt changes in climate, termed Dansgaard–Oeschger and Heinrich events, have
punctuated the last glacial period (∼ 100–10 kyr ago) but not the Holocene (the past 10 kyr) …

The possibility of a reduced Atlantic thermohaline circulation in response to increases in
greenhouse-gas concentrations has been demonstrated in a number of simulations with …

A faunal record of sea-surface temperature (SST) variations off West Africa documents a
series of abrupt, millennial-scale cooling events, which punctuated the Holocene warm …

Water vapor is a greenhouse gas that dominates Earth's terrestrial radiation absorption. As
the planetary temperature warms, forced by increasing CO 2 and other greenhouse gases …

Evaluating the significance of Holocene submillennial δ18O variability in the Greenland ice
cores is crucial for understanding how natural climate oscillations may modulate future …