| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2018NatCo...9.2947N |
| P5530 | Altmetric DOI | 10.1038/S41467-018-05312-3 |
| P6409 | CORE ID | 159113130 |
| P6179 | Dimensions Publication ID | 1105781321 |
| P356 | DOI | 10.1038/S41467-018-05312-3 |
| P953 | full work available at URL | http://eprints.whiterose.ac.uk/132789 |
| https://doi.org/10.1038/s41467-018-05312-3 | ||
| P6366 | Microsoft Academic ID | 2819534628 |
| P932 | PMC publication ID | 6063924 |
| P698 | PubMed publication ID | 30054472 |
| P1154 | Scopus EID | 2-s2.0-85050807206 |
| P50 | author | Laura Robinson | Q21264244 |
| Lauren J. Gregoire | Q56421003 | ||
| Ruza F. Ivanovic | Q56448503 | ||
| Hong Chin Ng | Q58477875 | ||
| Allison Jacobel | Q59674957 | ||
| P2093 | author name string | Jerry F McManus | |
| Tianyu Chen | |||
| Kais J Mohamed | |||
| P2860 | cites work | IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP | Q22255462 |
| Sea level and global ice volumes from the Last Glacial Maximum to the Holocene | Q28652807 | ||
| Ice-shelf collapse from subsurface warming as a trigger for Heinrich events | Q28741288 | ||
| Abrupt glacial climate shifts controlled by ice sheet changes | Q30842427 | ||
| Icebergs not the trigger for North Atlantic cold events | Q30932879 | ||
| Abrupt Bølling warming and ice saddle collapse contributions to the Meltwater Pulse 1a rapid sea level rise | Q31138600 | ||
| The Atlantic Meridional Overturning Circulation and Abrupt Climate Change. | Q31140939 | ||
| Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes | Q34315674 | ||
| High-resolution record of Northern Hemisphere climate extending into the last interglacial period | Q34346930 | ||
| Arctic freshwater forcing of the Younger Dryas cold reversal | Q34423312 | ||
| Early reactivation of European rivers during the last deglaciation | Q34566249 | ||
| A 0.5-million-year record of millennial-scale climate variability in the north atlantic | Q38547362 | ||
| Centennial-scale changes in the global carbon cycle during the last deglaciation | Q39106255 | ||
| Deglacial pulses of deep-ocean silicate into the subtropical North Atlantic Ocean. | Q39239136 | ||
| Reversed flow of Atlantic deep water during the Last Glacial Maximum | Q39298153 | ||
| Synchronous centennial abrupt events in the ocean and atmosphere during the last deglaciation | Q40503788 | ||
| 231Pa/230Th evidence for a weakened but persistent Atlantic meridional overturning circulation during Heinrich Stadial 1. | Q41675828 | ||
| Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warming | Q41995144 | ||
| The Southern Ocean's role in carbon exchange during the last deglaciation | Q43529277 | ||
| Absence of deep-water formation in the Labrador Sea during the last interglacial period | Q43927417 | ||
| Radiocarbon variability in the western North Atlantic during the last deglaciation | Q45167048 | ||
| Ocean mixing and ice-sheet control of seawater 234U/238U during the last deglaciation | Q47184213 | ||
| Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation | Q47211837 | ||
| Synchronous deglacial overturning and water mass source changes | Q47266485 | ||
| Bayesian Analysis of Radiocarbon Dates | Q54864766 | ||
| Massive iceberg discharges as triggers for global climate change | Q55933267 | ||
| Distinct roles of the Southern Ocean and North Atlantic in the deglacial atmospheric radiocarbon decline | Q56137020 | ||
| Abrupt North Atlantic circulation changes in response to gradual CO2 forcing in a glacial climate state | Q56431769 | ||
| How did the hydrologic cycle respond to the two-phase mystery interval? | Q56689732 | ||
| Deposition models for chronological records | Q57262905 | ||
| Accelerated drawdown of meridional overturning in the late-glacial Atlantic triggered by transient pre-H event freshwater perturbation | Q57532803 | ||
| High resolution evidence for linkages between NW European ice sheet instability and Atlantic Meridional Overturning Circulation | Q57532814 | ||
| Controls on seawater 231Pa, 230Th and 232Th concentrations along the flow paths of deep waters in the Southwest Atlantic | Q57812832 | ||
| Improved determination of marine sedimentation rates using230Thxs | Q57812948 | ||
| Interpretation of the 231Pa/230Th paleocirculation proxy: New water-column measurements from the southwest Indian Ocean | Q57813201 | ||
| Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings | Q58090254 | ||
| Deep water provenance and dynamics of the (de)glacial Atlantic meridional overturning circulation | Q58106071 | ||
| Observed decline of the Atlantic meridional overturning circulation 2004–2012 | Q58237760 | ||
| Muted change in Atlantic overturning circulation over some glacial-aged Heinrich events | Q58239133 | ||
| Synchronous and proportional deglacial changes in Atlantic meridional overturning and northeast Brazilian precipitation | Q58309634 | ||
| GEOTRACES intercalibration of230Th,232Th,231Pa, and prospects for10Be | Q58402504 | ||
| Anatomy of Heinrich Layer 1 and its role in the last deglaciation | Q58413628 | ||
| Millennial-scale fluctuations of the European Ice Sheet at the end of the last glacial, and their potential impact on global climate | Q59391144 | ||
| The first estimation of Fleuve Manche palaeoriver discharge during the last deglaciation: Evidence for Fennoscandian ice sheet meltwater flow in the English Channel ca 20–18ka ago | Q59391165 | ||
| Improvements to 232-thorium, 230-thorium, and 231-protactinium analysis in seawater arising from GEOTRACES intercalibration | Q59768337 | ||
| Opal burial in the equatorial Atlantic Ocean over the last 30 ka: Implications for glacial-interglacial changes in the ocean silicon cycle | Q59768350 | ||
| New insights into cycling of 231 Pa and 230 Th in the Atlantic Ocean | Q59813739 | ||
| Acceleration of Northern Ice Sheet Melt Induces AMOC Slowdown and Northern Cooling in Simulations of the Early Last Deglaciation | Q59882828 | ||
| Multiple causes of the Younger Dryas cold period | Q63970637 | ||
| Water mass properties and exchange between the Nordic seas and the northern North Atlantic during the period 23-6 ka: Benthic oxygen isotopic evidence | Q107105019 | ||
| P275 | copyright license | Creative Commons Attribution 4.0 International | Q20007257 |
| P6216 | copyright status | copyrighted | Q50423863 |
| P433 | issue | 1 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | general chemistry | Q909510 |
| P304 | page(s) | 2947 | |
| P577 | publication date | 2018-07-27 | |
| P1433 | published in | Nature Communications | Q573880 |
| P1476 | title | Coherent deglacial changes in western Atlantic Ocean circulation | |
| P478 | volume | 9 |
| Q59882828 | Acceleration of Northern Ice Sheet Melt Induces AMOC Slowdown and Northern Cooling in Simulations of the Early Last Deglaciation |
| Q64072019 | Deep-water circulation changes lead North Atlantic climate during deglaciation |
| Q59768291 | Paleoproductivity and Stratification Across the Subarctic Pacific Over Glacial-Interglacial Cycles |
| Q90057188 | The role of Northeast Pacific meltwater events in deglacial climate change |
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