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- 1From:Geochronology (Vol. 4, Issue 2) Peer-ReviewedAlpine glaciers in the western United States are often associated with late Holocene Little Ice Age (LIA) advances. Yet, recent studies have shown many of these glacial landforms are remnants of latest Pleistocene...
- 2From:Canadian Journal of Earth Sciences (Vol. 58, Issue 10) Peer-ReviewedA new [.sup.40Ar]/[.sup.39Ar] date from a pyroclastic density current deposit preserved on the northern slopes of the Lillooet River valley, British Columbia, indicates an explosive volcanic eruption of the Mount Meager...
- 3From:Bulletin of the American Meteorological Society (Vol. 101, Issue 5) Peer-ReviewedResearchers modeled the floodwater's movement during deglaciation that occurred 10,000-20,000 years ago. After traveling along the Columbia River, the flow mostly followed the coastline north, with some water crossing...
- 4From:Nature (Vol. 578, Issue 7795) Peer-ReviewedIn 1990, an oceanographer who had never worked on climate science proposed that ice-age cooling has been amplified by increased concentrations of iron in the sea -- and instigated an explosion of research. A historic...
- 5From:Climate of the Past (Vol. 15, Issue 5) Peer-Reviewed
We review paleoceanographic and paleoclimatic records from the northern North Atlantic to assess the nature of climatic conditions at 4.2 ka BP, which has been identified as a time of exceptional...
- 6From:Nature (Vol. 570, Issue 7759) Peer-ReviewedPlate tectonics is among the most important geological processes on Earth, but its emergence and evolution remain unclear. Here we extrapolate models of present-day plate tectonics to the past and propose that since...
- 7From:Climate of the Past (Vol. 15, Issue 1) Peer-Reviewed
Constraining Antarctica's climate evolution since the end of the Last Glacial Maximum (â¼18 ka) remains a key challenge, but is important for accurately projecting future changes in Antarctic...
- 8From:Climate of the Past (Vol. 15, Issue 1) Peer-Reviewed
Strong similarities in Holocene climate reconstructions derived from multiple proxies (BSi, TOC - total organic carbon, [delta].sup.13 C, C/N, MS - magnetic susceptibility, [delta].sup.15 N) preserved in sediments...
- 9From:PeerJ (Vol. 6) Peer-ReviewedQuaternary climatic oscillations have impacted Patagonian sigmodontine fauna, leaving traceable genetic footprints. In southern Chile, changes in the landscape included transitions to different vegetation formations as...
- 10From:Climate of the Past (Vol. 14, Issue 12) Peer-Reviewed
We have developed a new module to calculate soil organic carbon (SOC) accumulation in perennially frozen ground in the land surface model JSBACH. Running this offline version of MPI-ESM we have modelled long-term...
- 11From:Climate of the Past (Vol. 14, Issue 12) Peer-Reviewed
A radiocarbon-dated marine sediment core retrieved in Kane Basin, central Nares Strait, was analysed to constrain the timing of the postglacial opening of this Arctic gateway and its Holocene evolution. This study is...
- 12From:The Cryosphere (Vol. 12, Issue 12) Peer-Reviewed
A set of supraglacial ponds filled rapidly between April and July 2017 on Changri Shar Glacier in the Everest region of Nepal, coalescing into a â¼180 000 m.sup.2 lake before sudden and...
- 13From:Canadian Journal of Earth Sciences (Vol. 55, Issue 12) Peer-ReviewedIn the past, researchers have disagreed over the maximum extent of the Cordilleran Ice Sheet in the Peace River valley during the Late Wisconsinan. Some workers argued that Cordilleran ice reached beyond the Rocky...
- 14From:Geoscientific Model Development (Vol. 11, Issue 11) Peer-Reviewed
As ice sheets grow or decay, the net flux of freshwater into the ocean changes and the bedrock adjusts due to isostatic adjustments, leading to variations in the bottom topography and the oceanic boundaries. This...
- 15From:Climate of the Past (Vol. 14, Issue 10) Peer-Reviewed
Over the past 0.8 million years, 100 kyr ice ages have dominated Earth's climate with geological evidence suggesting the last glacial inception began in the mountains of Baffin Island. Currently,...
- 16From:The Cryosphere (Vol. 12, Issue 10) Peer-Reviewed
The European Alps, the cradle of pioneering glacial studies, are one of the regions where geological markers of past glaciations are most abundant and well-studied. Such conditions make the region ideal for testing...
- 17From:Earth Surface Dynamics (Vol. 6, Issue 3) Peer-Reviewed
During the Last Glacial Maximum (LGM), most of the major glaciated basins of the European Southern Alps had piedmont lobes with large outwash plains; only a few glaciers remained within the valley. Piedmont glaciers...
- 18From:Geographica Helvetica (Vol. 73, Issue 3) Peer-Reviewed
Exposure dating has substantially improved our knowledge about glacier advances during the Younger Dryas (YD) and the early Holocene. The glacier development after the Last Glacial Maximum (LGM) and the timing of...
- 19From:Earth System Dynamics (Vol. 9, Issue 3) Peer-Reviewed
Variations in Northern Hemisphere ice volume over the past 3 million years have been described in numerous studies and well documented. These studies depict the mid-Pleistocene transition from 40 kyr...
- 20From:Climate of the Past (Vol. 14, Issue 7) Peer-Reviewed
The late Pliocene/early Pleistocene intensification of Northern Hemisphere glaciation (iNHG) â¼ 2.5 million years ago (marine isotope stages, MIS, 100-96) stands out as an important tipping point in...