Stable carbon isotopes in paleoceanography: atmosphere, oceans, and sediments
Carbon is one of the key elements in organisms and non-living compounds on Earth.
Carbon dioxide and methane are important greenhouse gases in the atmosphere, dissolved …
Carbon dioxide and methane are important greenhouse gases in the atmosphere, dissolved …
Radiocarbon as a dating tool and tracer in paleoceanography
LC Skinner, E Bard - Reviews of Geophysics, 2022 - Wiley Online Library
Radiocarbon is an extremely useful carbon cycle tracer and radiometric dating tool. Here,
we review the main principles and challenges involved in the use of radiocarbon in …
we review the main principles and challenges involved in the use of radiocarbon in …
Reducing uncertainties in carbonate clumped isotope analysis through consistent carbonate‐based standardization
About a decade after its introduction, the field of carbonate clumped isotope thermometry is
rapidly expanding because of the large number of possible applications and its potential to …
rapidly expanding because of the large number of possible applications and its potential to …
Radiocarbon constraints on the glacial ocean circulation and its impact on atmospheric CO2
LC Skinner, F Primeau, E Freeman… - Nature …, 2017 - nature.com
While the ocean's large-scale overturning circulation is thought to have been significantly
different under the climatic conditions of the Last Glacial Maximum (LGM), the exact nature …
different under the climatic conditions of the Last Glacial Maximum (LGM), the exact nature …
Deglacial floods in the Beaufort Sea preceded Younger Dryas cooling
A period of cooling about 13,000 years ago interrupted about 2,000 years of deglacial
warming. Known as the Younger Dryas (YD), the event is thought to have resulted from a …
warming. Known as the Younger Dryas (YD), the event is thought to have resulted from a …
Evolution of the Global Overturning Circulation since the Last Glacial Maximum based on marine authigenic neodymium isotopes
Abstract The Global Overturning Circulation is linked to climate change on glacial-
interglacial and multi-millennial timescales. The understanding of past climate-circulation …
interglacial and multi-millennial timescales. The understanding of past climate-circulation …
Controls on the stable isotope compositions of travertine from hyperalkaline springs in Oman: Insights from clumped isotope measurements
Carbonate formation at hyperalkaline springs is typical of serpentinization in peridotite
massifs worldwide. These travertines have long been known to exhibit large variations in …
massifs worldwide. These travertines have long been known to exhibit large variations in …
Warm deep-sea temperatures across Eocene Thermal Maximum 2 from clumped isotope thermometry
The early Eocene hothouse experienced highly elevated atmospheric CO2 levels and
multiple transient global warming events, so-called hyperthermals. The deep ocean …
multiple transient global warming events, so-called hyperthermals. The deep ocean …
Deep-water circulation changes lead North Atlantic climate during deglaciation
Constraining the response time of the climate system to changes in North Atlantic Deep
Water (NADW) formation is fundamental to improving climate and Atlantic Meridional …
Water (NADW) formation is fundamental to improving climate and Atlantic Meridional …
The North Atlantic Glacial Eastern Boundary Current as a key driver for ice‐sheet—AMOC interactions and climate instability
The upper branch of the Atlantic meridional overturning circulation (AMOC) plays a critical
role in ocean circulation and climate change, yet its variability during the last glacial period …
role in ocean circulation and climate change, yet its variability during the last glacial period …