Plio-Pleistocene deep-sea ventilation in the Eastern Pacific and potential linkages with Northern Hemisphere glaciation
Antarctic bottom water (AABW) production is a key factor governing global ocean circulation,
and the present disintegration of the Antarctic Ice Sheet slows it. However, its long-term …
and the present disintegration of the Antarctic Ice Sheet slows it. However, its long-term …
Diverse glacial ventilation in deep Pacific: An integrated record from Mariana Trench and Magellan Seamounts over last 1.2 Myr
L Yi - Global and Planetary Change, 2023 - Elsevier
Antarctic bottom water production is one of the most important components in oceanic
circulation, yet its long-term impact on Earth's climate remains poorly known. In this study …
circulation, yet its long-term impact on Earth's climate remains poorly known. In this study …
Increased ventilation of Antarctic deep water during the warm mid-Pliocene
The mid-Pliocene warm period is a recent warm geological period that shares similarities
with predictions of future climate. It is generally held the mid-Pliocene Atlantic Meridional …
with predictions of future climate. It is generally held the mid-Pliocene Atlantic Meridional …
Changes in Pacific Ocean circulation following the Miocene onset of permanent Antarctic ice cover
We integrate micropaleontological and geochemical records (benthic stable isotopes,
neodymium isotopes, benthic foraminiferal abundances and XRF-scanner derived …
neodymium isotopes, benthic foraminiferal abundances and XRF-scanner derived …
Controls on deglacial changes in biogenic fluxes in the North Pacific Ocean
KE Kohfeld, Z Chase - Quaternary Science Reviews, 2011 - Elsevier
The subarctic North Pacific Ocean holds a large CO2 reservoir that is currently isolated from
the atmosphere by a low-salinity layer. It has recently been hypothesized that the …
the atmosphere by a low-salinity layer. It has recently been hypothesized that the …
Ventilation and expansion of intermediate and deep waters in the Southeast Pacific during the last termination
We investigate the geometry and ventilation of the water masses within bathyal depths (~
1,500 to~ 2,500 m) of the Southeast Pacific (SEP), inferring the lower depth limit variations of …
1,500 to~ 2,500 m) of the Southeast Pacific (SEP), inferring the lower depth limit variations of …
Oxygenated deep waters fed early Atlantic overturning circulation upon Antarctic glaciation
The Atlantic meridional overturning circulation (AMOC) exerts a major control on the global
distribution of heat, dissolved oxygen and carbon in the ocean. Yet the timing and cause of …
distribution of heat, dissolved oxygen and carbon in the ocean. Yet the timing and cause of …
Impact of Antarctic Circumpolar Current development on late Paleogene ocean structure
ME Katz, BS Cramer, JR Toggweiler, G Esmay, C Liu… - Science, 2011 - science.org
Global cooling and the development of continental-scale Antarctic glaciation occurred in the
late middle Eocene to early Oligocene (~ 38 to 28 million years ago), accompanied by deep …
late middle Eocene to early Oligocene (~ 38 to 28 million years ago), accompanied by deep …
Reorganization of Pacific Deep Waters linked to middle Miocene Antarctic cryosphere expansion: A perspective from the South China Sea
J Tian, A Shevenell, P Wang, Q Zhao, Q Li… - Palaeogeography …, 2009 - Elsevier
Changes in intermediate and deep ocean circulation likely played a significant role in global
carbon cycling and meridional heat/moisture transport during the middle Miocene climate …
carbon cycling and meridional heat/moisture transport during the middle Miocene climate …
Deepwater formation in the North Pacific during the last glacial termination
Between~ 17,500 and 15,000 years ago, the Atlantic meridional overturning circulation
weakened substantially in response to meltwater discharges from disintegrating Northern …
weakened substantially in response to meltwater discharges from disintegrating Northern …