scholarly article | Q13442814 |
P356 | DOI | 10.1038/NGEO2045 |
P50 | author | Rong Zhang | Q56854872 |
Stefan Mulitza | Q57907197 | ||
Jean Lynch-Stieglitz | Q58109957 | ||
P2093 | author name string | Ping Chang | |
William B. Curry | |||
Luke C. Skinner | |||
Matthew W. Schmidt | |||
L. Gene Henry | |||
P2860 | cites work | Impact of abrupt deglacial climate change on tropical Atlantic subsurface temperatures. | Q30558539 |
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Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes | Q34315674 | ||
Atlantic meridional overturning circulation during the Last Glacial Maximum | Q36782592 | ||
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Coherent high- and low-latitude control of the northwest African hydrological balance | Q56655912 | ||
Onset of “Hudson Strait” Heinrich events in the eastern North Atlantic at the end of the middle Pleistocene transition (∼640 ka)? | Q56854406 | ||
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IntCal09 and Marine09 Radiocarbon Age Calibration Curves, 0–50,000 Years cal BP | Q57262902 | ||
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Oceanic link between abrupt changes in the North Atlantic Ocean and the African monsoon | Q58239150 | ||
Simulated Tropical Response to a Substantial Weakening of the Atlantic Thermohaline Circulation | Q58239159 | ||
Testing the impact of seasonal phytodetritus deposition on δ13C of epibenthic foraminifer Cibicidoides wuellerstorfi: A 31,000 year high-resolution record from the northwest African continental slope | Q58309677 | ||
Potential links between surging ice sheets, circulation changes, and the Dansgaard-Oeschger Cycles in the Irminger Sea, 60-18 Kyr | Q58617231 | ||
Weaker Gulf Stream in the Florida Straits during the Last Glacial Maximum | Q59068682 | ||
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P433 | issue | 2 | |
P407 | language of work or name | English | Q1860 |
P921 | main subject | Heinrich event | Q1596382 |
Atlantic meridional overturning circulation | Q4652675 | ||
P304 | page(s) | 144-150 | |
P577 | publication date | 2014-01-12 | |
P1433 | published in | Nature Geoscience | Q1337483 |
P1476 | title | Muted change in Atlantic overturning circulation over some glacial-aged Heinrich events | |
P478 | volume | 7 |
Q58090120 | Abrupt changes in the southern extent of North Atlantic Deep Water during Dansgaard–Oeschger events |
Q58403804 | Assessing reconstruction techniques of the Atlantic Ocean circulation variability during the last millennium |
Q105427035 | Assessing the Ability of Zonal δ 18 O Contrast in Benthic Foraminifera to Reconstruct Deglacial Evolution of Atlantic Meridional Overturning Circulation |
Q58054863 | Calibration of the carbon isotope composition (δ13 C) of benthic foraminifera |
Q58422093 | Coherent deglacial changes in western Atlantic Ocean circulation |
Q93064066 | Consistently dated Atlantic sediment cores over the last 40 thousand years |
Q58073979 | Data Constraints on Glacial Atlantic Water Mass Geometry and Properties |
Q64072019 | Deep-water circulation changes lead North Atlantic climate during deglaciation |
Q31111700 | North Atlantic ocean circulation and abrupt climate change during the last glaciation |
Q47184213 | Ocean mixing and ice-sheet control of seawater 234U/238U during the last deglaciation |
Q59813721 | Past Carbonate Preservation Events in the Deep Southeast Atlantic Ocean (Cape Basin) and Their Implications for Atlantic Overturning Dynamics and Marine Carbon Cycling |
Q28602545 | Punctuated Shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 |
Q41196934 | Rapid global ocean-atmosphere response to Southern Ocean freshening during the last glacial. |
Q58090100 | Strong middepth warming and weak radiocarbon imprints in the equatorial Atlantic during Heinrich 1 and Younger Dryas |
Q58309634 | Synchronous and proportional deglacial changes in Atlantic meridional overturning and northeast Brazilian precipitation |
Q41321535 | Synchronous precipitation reduction in the American Tropics associated with Heinrich 2 |
Q100945863 | The fast-acting "pulse" of Heinrich Stadial 3 in a mid-latitude boreal ecosystem |
Q30867340 | Topography's crucial role in Heinrich Events |
Q58309632 | Variability in mid-depth ventilation of the western Atlantic Ocean during the last deglaciation |
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