Compared with the widely used stable oxygen isotope (δ 18 O), the climate response of the
stable carbon isotope (δ 13 C) of speleothems in monsoonal China has received less …

Brazil has a megadiversity that includes marine species that are distributed along 800 km of
shoreline. This biodiversity status holds promising biotechnological potential. Marine …

Although reef coral skeletal carbon isotopes (δ13C) are routinely measured, interpretation
remains controversial. Here we show results of a consistent inverse relationship between …

Geological records of seasonal sea surface temperature (SST) records are useful for better
understanding the past dynamics of coastal upwelling, and for inferring future scenarios. By …

Abstract The 2–7-year periodicities recorded in fossil coral records have been widely used
to identify paleo-El Niño events. However, the reliability of this approach in the South China …

Boron systematics offer a unique opportunity to reveal coral calcifying fluid (CF) chemistry
and seawater pH (pHsw). Here, we assess the intercolony differences of skeletal δ11B and …

This investigation into the Little Ice Age (LIA) climate discrepancies explores sea surface
temperature (SST) anomalies in the South China Sea (SCS) using monthly resolved coral …

To better understand the effect of human activities on tropical oceanic climate change,
existing coral-based paleoclimate data from the northern South China Sea (SCS) for several …

The geochemistry preserved in massive scleractinian corals has long been used as proxies
for river runoff, but its reliability in naturally extreme environment (ie, strong hydrodynamics …

The decadal variability of ocean primary productivity (PP) has mainly been studied using
relatively short term satellite data, limiting its in‐depth analysis. Here, by removing the …