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Cosmogenic evidence for limited local LGM glacial expansion, Denton Hills, Antarctica
(Elsevier, 2017)
The geomorphology of the Denton Hills provides insight into the timing and magnitude of glacial retreats
in a region of Antarctica isolated from the influence of the East Antarctic ice sheet. We present 26
Beryllium-10 ...
Dust fluxes and iron fertilization in Holocene and Last Glacial Maximum climates
(Amer Geophysical Union, 2015)
Mineral dust aerosols play a major role in present and past climates. To date, we rely on climate
models for estimates of dust fluxes to calculate the impact of airborne micronutrients on
biogeochemical cycles. Here we ...
The PMIP4 contribution to CMIP6-Part 4: Scientific objectives and experimental design of the PMIP4-CMIP6 Last Glacial Maximum experiments and PMIP4 sensitivity experiments
(2017)
The Last Glacial Maximum (LGM, 21 000 years ago) is one of the suite of paleoclimate simulations included in the current phase of the Coupled Model Intercomparison Project (CMIP6). It is an interval when insolation was ...
Cosmogenic evidence for limited local LGM glacial expansion, Denton Hills, Antarctica
(2017)
The geomorphology of the Denton Hills provides insight into the timing and magnitude of glacial retreats in a region of Antarctica isolated from the influence of the East Antarctic ice sheet. We present 26 Beryllium-10 surface ...
Sensitivity of Southern Hemisphere circulation to LGM and 4
(American Geophysical Union, 2013)
The Alpine LGM in the boreal ice-sheets game
(Nature Publishing Group, 2017-05-18)
New chronologic and stratigraphic constraints from the Garda morainic amphitheater define the extension of the last glaciation in the Adige-Sarca system and improve the Alpine LGM dataset. Together with the available ...
Simultaneous occurrence of Hb C trait and polycythaemia vera
(Revista de Biologia Tropical, 2014)
Palaeoceanography of the last glacial maximum in the eastern Indian Ocean: Planktonic foraminiferal evidence
(ELSEVIER SCIENCE BV, 1999-01-01)
Palaeoceanographic conditions in the eastern Indian Ocean for the last ~30 kyr are documented by means of planktonic foraminiferal analyses of 10 gravity cores. Quantitative foraminiferal analysis (%), Q-mode factor analysis, ...