Carbon preservation in marine sediments, supplemented by that in large lakes, is the
primary mechanism that moves carbon from the active surficial carbon cycle to the slower …

A growing body of evidence suggests that respired carbon was stored in mid-depth waters
(∼ 1–3 km) during the last glacial maximum (LGM) and released to the atmosphere from …

The coupled 100,000 year variations in ice volume, temperature, and atmospheric CO 2
during the late Pleistocene are generally considered to arise from a combination of orbital …

As the largest reservoir of carbon exchanging with the atmosphere on glacial–interglacial
timescales, the deep ocean has been implicated as the likely location of carbon …

The ocean plays a critical role in the global climate by modulating atmospheric CO 2 via
carbon exchange between the atmosphere and the ocean, a process tightly linked to ocean …

Records of carbonate ion concentration ([CO 3 2−]) and benthic carbon isotope (δ 13 C)
have profound implications for exploring deep water circulation and global carbon cycle …

Sedimentation rate, bioturbation, winnowing, and calcite dissolution produce significant
radiocarbon age offsets among multiple species of coexisting planktonic foraminifers and …

We present a new deep‐water carbonate ion concentration ([CO32−]) record, reconstructed
from the “size‐normalized weight” of the planktonic foraminifer Neogloboquadrina dutertrei …

Late Quaternary carbonate dissolution was evaluated by using planktonic foraminifera
indices perfect test ratio (PTR) of Goborotalia menardii, G. menardii fragmentation index …

Abstract The Eastern Equatorial Pacific (EEP) affects the ocean-atmosphere exchange of
CO 2 on seasonal and interannual time scales through a balance of upwelling of CO 2-rich …