The ocean absorbs> 90% of anthropogenic heat in the Earth system, moderating global
atmospheric warming. However, it remains unclear how this heat uptake is distributed by …

Using in situ data from 88 cruises from 1987 to 2009 in the East China Sea, downstream
nutrient flux (the product of velocity and nutrient concentration) and nutrient transport …

Evidence from geochemical tracers (salinity, oxygen, silicate, nutrients, alkalinity, dissolved
inorganic carbon (DIC), carbon isotopes (δ13CDIC) and radiocarbon (Δ14C)) collected …

Neodymium isotopic compositions (εNd) and rare earth element (REE) concentrations were
measured for filtered surface to deep waters (112 samples) in the Southern Tropical Pacific …

In a modeling sensitivity study we investigate the evolution of the ocean circulation and of
marine carbon isotope (δ13C) records during the Miocene (about 23–5 million years ago) …

Recent in situ observations of chromophoric dissolved organic material (CDOM) in the
Pacific Ocean reveal the biogeochemical controls on CDOM and indicate predictive …

In the Atlantic, where deep circulation is vigorous, the dissolved neodymium (Nd) isotopic
composition (expressed as ɛ Nd) is largely controlled by water mass mixing. In contrast, the …

It has been speculated that the subtropical North Pacific Intermediate Water (NPIW) was
formed by a shortcut of Okhotsk Sea source into the western subtropical gyre because this is …

The deep-ocean carbon cycle, especially carbon sequestration and outgassing, is one of the
mechanisms to explain variations in atmospheric CO 2 concentrations on millennial and …

Chromophoric dissolved organic matter (CDOM) was surveyed along the 160° W transect
from the equatorial to the subarctic Pacific. CDOM characteristics were evaluated through …