Glacial–interglacial climate cycles are known to have triggered migrations and
reassortments of tropical biota. Although long-term precessionally-driven changes in …

During the Pleistocene, long-term trends in global climate were controlled by orbital cycles
leading to high amplitude glacial-interglacial variability. The history of Amazonian vegetation …

Understanding the influence of future sea-level rise (SLR) on coastal ecosystems is
improved by examining response of coastlines during historic periods of SLR. We evaluated …

We report stable isotope, core scanning XRF, and ice-rafted detritus (IRD) data in glacial-
aged sediments from piston Core KN166-14-JPC-13 (hereafter referred to as JPC-13) …

Quaternary sediment of the South Yellow Sea (SYS) is usually assumed to record climatic
changes, tectonic activities and major river evolutions. However, as an important terrigenous …

To reconstruct the response of vegetation to abrupt climate changes during the last glacial
we have compiled pollen records from the circum-Atlantic tropics between 23° N and 23° S …

Exposure of the presently submerged continental shelf of Southeast Asia during low sea-
level stands of the Quaternary is thought to be deeply involved in the biogeographic …

Over the last glacial cycle, climate variations in the Neotropics were related to diverse
forcing mechanisms whose understanding has been limited because of the scarcity of …

This paper analyzes the diversification of the Neotropical mangrove flora from the Miocene
to the present, using a fairly comprehensive database of 110 pollen records distributed …

Local geomorphology plays an important role in the response of mangrove communities to
both sea-level rise and precipitation changes, mostly because it exerts an important control …