Paleoclimatic records show that the Greenland Ice Sheet consistently has lost mass in response to warming, and grown in response to cooling. Such changes have occurred even …
There have been significant changes in sea level over the past two million years, and a complete understanding of natural cycles of change as well as anthropogenic effects is …
HA Bauch, H Erlenkeuser, RF Spielhagen… - Quaternary Science …, 2001 - Elsevier
On the basis of various lithological, mircopaleontological and isotopic proxy records covering the last 30,000 calendar years (cal kyr) the paleoenvironmental evolution of the …
I Candy, DC Schreve, J Sherriff, GJ Tye - Earth-Science Reviews, 2014 - Elsevier
Abstract Interglacials of the Quaternary Period are currently the focus of a great deal of attention within the scientific community. This is primarily because they play a vital role in …
In an attempt to find potential interglacial analogues of our present interglacial and its natural future, five interglacials (MIS-1, 5, 9, 11 and 19) are studied in terms of their …
Stable isotope and ice-rafted debris records from three core sites in the mid-latitude North Atlantic (IODP Site U1313, MD01-2446, MD03-2699) are combined with records of ODP …
S Becquey, R Gersonde - Palaeogeography, Palaeoclimatology …, 2002 - Elsevier
Pleistocene summer sea-surface temperatures (SSST) have been reconstructed on a composite core section recovered in the Subantarctic Zone of the Southern Ocean from …
S Barker, D Archer, L Booth, H Elderfield… - Quaternary Science …, 2006 - Elsevier
The Mid-Brunhes dissolution interval (MBDI) represents a period of global carbonate dissolution, lasting several hundred thousand years, centred around Marine Isotope Stage …
Pleistocene interglacials are often considered to be possible geological analogs for the climatic development of the Holocene epoch. Marine isotope stage 11 (MIS 11), a prominent …