| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2014NatGe...7..109R |
| P356 | DOI | 10.1038/NGEO2053 |
| P5875 | ResearchGate publication ID | 261016199 |
| P50 | author | Dirk Sachse | Q58084402 |
| P2093 | author name string | A. Brauer | |
| H. Wilkes | |||
| O. Rach | |||
| P2860 | cites work | High-resolution Greenland ice core data show abrupt climate change happens in few years | Q31159882 |
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| Leaf epicuticular waxes. | Q54290653 | ||
| Molecular Paleohydrology: Interpreting the Hydrogen-Isotopic Composition of Lipid Biomarkers from Photosynthesizing Organisms | Q55113347 | ||
| Tellus A: Dynamic Meteorology and Oceanography, Volume 73, Issue 1 (2021) | Q55920089 | ||
| Synchronized TerrestrialAtmospheric Deglacial Records Around the North Atlantic | Q55951110 | ||
| The abrupt termination of the Younger Dryas climate event | Q56092734 | ||
| An abrupt wind shift in western Europe at the onset of the Younger Dryas cold period | Q56092782 | ||
| Volcanic ash reveals time-transgressive abrupt climate change during the Younger Dryas | Q56092784 | ||
| High resolution sediment and vegetation responses to Younger Dryas climate change in varved lake sediments from Meerfelder Maar, Germany | Q56680405 | ||
| δD values of individual n-alkanes from terrestrial plants along a climatic gradient – Implications for the sedimentary biomarker record | Q56698120 | ||
| Freshwater outbursts to the oceans from glacial Lake Agassiz and their role in climate change during the last deglaciation | Q56804398 | ||
| A new Greenland ice core chronology for the last glacial termination | Q57242109 | ||
| δD values of n-alkanes in Tibetan lake sediments and aquatic macrophytes – A surface sediment study and application to a 16ka record from Lake Koucha | Q58086348 | ||
| Water vapour source impacts on oxygen isotope variability in tropical precipitation during Heinrich events | Q58307060 | ||
| Production of n-alkyl lipids in living plants and implications for the geologic past | Q58319960 | ||
| Leaf water deuterium enrichment shapes leaf wax n-alkane δD values of angiosperm plants II: Observational evidence and global implications | Q60120480 | ||
| Lateglacial summer temperatures in the Northwest European lowlands: a chironomid record from Hijkermeer, the Netherlands | Q63970663 | ||
| A Mid-European Decadal Isotope-Climate Record from 15,500 to 5000 Years B.P. | Q63971546 | ||
| P433 | issue | 2 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | Greenland | Q223 |
| Younger Dryas | Q944279 | ||
| Western Europe | Q27496 | ||
| P304 | page(s) | 109-112 | |
| P577 | publication date | 2014-01-19 | |
| P1433 | published in | Nature Geoscience | Q1337483 |
| P1476 | title | Delayed hydrological response to Greenland cooling at the onset of the Younger Dryas in western Europe | |
| P478 | volume | 7 |
| Q57892250 | A dual-biomarker approach for quantification of changes in relative humidity from sedimentary lipid D∕H ratios |
| Q117157001 | Concept and global context of the glacial landforms from the Younger Dryas Stadial |
| Q59392545 | Cosmic-Impact Event in Lake Sediments from Central Europe Postdates the Laacher See Eruption and Marks Onset of the Younger Dryas |
| Q57946429 | Decadally Resolved Lateglacial Radiocarbon Evidence from New Zealand Kauri |
| Q64072019 | Deep-water circulation changes lead North Atlantic climate during deglaciation |
| Q47186798 | Did thermophilous trees spread into central Europe during the Late Glacial? |
| Q56092781 | Evaluating the link between the sulfur-rich Laacher See volcanic eruption and the Younger Dryas climate anomaly |
| Q28607055 | Fennoscandian freshwater control on Greenland hydroclimate shifts at the onset of the Younger Dryas |
| Q63970903 | Lags within the Younger Dryas |
| Q57881000 | Leaf wax biomarkers in transit record river catchment composition |
| Q35427910 | Major evolutionary trends in hydrogen isotope fractionation of vascular plant leaf waxes |
| Q31120527 | Molecular Paleoclimate Reconstructions over the Last 9 ka from a Peat Sequence in South China |
| Q45016152 | Paleobotanical and climate data support the plausibility of temperate trees spread into central Europe during the Late Glacial |
| Q60120358 | Prolonged Monsoonal Moisture Availability Preconditioned Glaciation of the Tibetan Plateau During the Mid‐Pleistocene Transition |
| Q28602545 | Punctuated Shutdown of Atlantic Meridional Overturning Circulation during Greenland Stadial 1 |
| Q46719263 | Seasonal variation of leaf wax n-alkane production and δ(2)H values from the evergreen oak tree, Quercus agrifolia |
| Q58726222 | Subfossil trees suggest enhanced Mediterranean hydroclimate variability at the onset of the Younger Dryas |
| Q117157000 | Synchronous or Not? The Timing of the Younger Dryas and Greenland Stadial-1 Reviewed Using Tephrochronology |
| Q99233696 | Timing and structure of the Younger Dryas event and its underlying climate dynamics |
| Q28598035 | Validation of climate model-inferred regional temperature change for late-glacial Europe |
| Q58596215 | Vegetation development in south-east Denmark during the Weichselian Late Glacial: palaeoenvironmental studies close to the Palaeolithic site of Hasselø |
| Q52565498 | Warm summers during the Younger Dryas cold reversal. |
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