Jasmin M. Link
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View article: Expedition 397 summary
Expedition 397 summary Open
During International Ocean Discovery Program Expedition 397, we recovered a total of 6176.7 m of core (104.2%recovery) at four sites (U1586, U1587, U1385, and U1588) from the Promontório dos Príncipes de Avis, a plateau located on the Port…
View article: Expedition 397 methods
Expedition 397 methods Open
Common coring-induced deformation includes the concave-downward appearance of originally horizontal bedding.Piston action may result in fluidization (flow-in) at the bottom of, or sometimes in, APC cores.Retrieval of unconsolidated (APC) c…
View article: Large-scale Pacific-sourced intrusion into the glacial South Atlantic
Large-scale Pacific-sourced intrusion into the glacial South Atlantic Open
The deep Southern Ocean (SO) circulation plays a key role in the storage and release of CO2 in Earth’s climate system. Uptake and release of CO2 strongly depend on the redistribution of well and poorly ventilated water masses. Here, we pre…
View article: Persistent ISOW formation during MIS 11
Persistent ISOW formation during MIS 11 Open
<p>The deep water formation in the Labrador and Nordic Seas is crucial for the global thermohaline circulation nowadays and it remains debated whether changing boundary conditions in terms of global warming may influence the deep con…
View article: Dominance of Pacific Sourced Deep Water in the Atlantic sector of the Southern Ocean during the last glacials
Dominance of Pacific Sourced Deep Water in the Atlantic sector of the Southern Ocean during the last glacials Open
<p>The deep Southern Ocean (SO) circulation is of major significance for the understanding of the ocean&#180;s impact on Earth&#8217;s climate as uptake and release of CO<sub>&#173;&#173;&#173;2</sub> …
View article: Deep water circulation patterns in the Atlantic during MISs 12-11
Deep water circulation patterns in the Atlantic during MISs 12-11 Open
<p>Glacial Termination V is one of the most extreme glacial-interglacial transitions of the past 800 ka [1]. However, the changes in orbital forcing from Marine Isotope Stage (MIS) 12 to 11 are comparatively weak. In addition, MIS 11…
View article: Constraining the Variability of the Atlantic Meridional Overturning Circulation During the Holocene
Constraining the Variability of the Atlantic Meridional Overturning Circulation During the Holocene Open
There is a converging body of evidence supporting a measurable slowdown of the Atlantic Meridional Overturning Circulation (AMOC) as climate warms and Northern Hemisphere ice sheets inexorably shrink. Within this context, we assess the var…
View article: Influence of Ocean Circulation and Benthic Exchange on Deep Northwest Atlantic Nd Isotope Records During the Past 30,000 Years
Influence of Ocean Circulation and Benthic Exchange on Deep Northwest Atlantic Nd Isotope Records During the Past 30,000 Years Open
Neodymium (Nd) isotopes extracted from authigenic sediment phases are increasingly used as a proxy for past variations in water mass provenance. To better constrain the controls of water mass provenance and nonconservative effects on the a…
View article: High resolution paleocirculation records from the Bermuda Rise for the past 11,000 year
High resolution paleocirculation records from the Bermuda Rise for the past 11,000 year Open
We present a compilation of paleo-circulation proxies during the Holocene from Bermuda Rise core ODP Site 1063. The data set comprises high resolution 231Pa/230Th (including 231Pa,230Th, 232Th, and 238U concentrations accompanied by measur…