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The aim of this project was to conduct geological fieldwork on northeast Svalbard in order to collect lake sediment cores that might reveal the glacial and environmental history over the last c. An international field expedition to northeast Svalbard, supported by the Carlsberg Foundation, was undertaken in July-August We successfully obtained sediment cores from three threshold lakes.
The preliminary results reveal that the sediment cores contain a palaeo-environmental record back to the last deglaciation.
Studies covering the whole LIA period are limited. Absolute dating records are rare, and largely derived from Scoresby Sund, of the Lyngmarksbræen ice cap (°N; °W; 32 km2 in ), Marrero, S. M., Phillips, F. M., Caffee, M. W. & Gosse, J. C. CRONUS-Earth cosmogenic 36Cl calibration.
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highland individual (Llorente et al., ) and with SNP geno- Hammer, M.F., Woerner, A.E., Mendez, F.L., Watkins, J.C., and Wall, J.D. · (). Age (LIA) deposits dating to the last two thousand years (Helm et al., ).
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It is shown that Churup glacier has lost the vast majority of its estimated LIA extent 1. The rate of glacier retreat is documented to vary in space SE, SW and NW-facing slopes and time, with the peak between and With an area of 0.
Huntley DJ, Godfrey-Smith DI, Thewalt MLW () Optical dating of Radiat Meas – Kim JC, Chang TS, Ti S, Hong SS, Nahm WH () OSL dating OSL surface exposure dating to reconstruct post-LIA glacier fluctuations in the.
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historie · Tidslinie for Carlsbergfamilien · Tidslinje Brygger J.C. Jacobsen · J. C. For example, the Little Ice Age (LIA) is the best documented glacial and glacial landforms and deposits that pre-date the LIA moraines exist, yet little is located on the west coast of Spitsbergen (van der Bilt et al., ).
Normal kernel density estimates of 10 Be ages grouped by moraine from Baffin Island. We use cosmogenic beryllium dating to develop a moraine chronology with century-scale resolution over the last millennium and show that alpine glaciers in Baffin Island and western Greenland were at or near their maximum LIA configurations during the proposed general timing of the MWP. Complimentary paleoclimate proxy data suggest that the western North Atlantic region remained cool, whereas the eastern North Atlantic region was comparatively warmer during the MWP—a dipole pattern compatible with a persistent positive phase of the North Atlantic Oscillation.
These results demonstrate that over the last millennium, glaciers approached their eventual LIA maxima before what is considered the classic LIA in the Northern Hemisphere. Our results, paired with other regional climate records, point to nonclimatic factors as contributing to the Norse exodus from the western North Atlantic region. The perceived warmth of the MWP, with a North Atlantic climate favorable for sea voyage and increased crop yield, has often been invoked as a catalyst for Norse migration into the western North Atlantic region 8 , 9.
Reasons behind initial Norse settlement and eventual demise remain controversial; some suggest that mild conditions and decreased sea ice during the MWP, followed by deteriorating climate during the LIA, were the primary factors influencing Norse migration patterns 14 , 15 , whereas others note Norse resilience and suggest that alternative socioeconomic factors, such as a decrease in Norse shipping and trading opportunities, led to the Norse leaving their Greenland settlements 16 , Developing robust regional records of climate variability that span the MWP-LIA interval can help determine which climatic mechanisms drive regional centennial- to subcentennial-scale climate variability, and can provide a fundamental framework to evaluate Norse cultural adaptations to key climate system changes.
Glaciers are highly sensitive to changes in temperature and precipitation 18 , and accordingly, past fluctuations in glacier extent can be used to robustly reconstruct past changes in climate. Where glacier termini intersect tree line, precise glacier histories that span millennia can be reconstructed 19 , but unfortunately, Arctic glaciers have not intersected tree line during the late Holocene.
Hence, reconstructing Arctic glacier change has proven difficult. Moraines deposited on the landscape mark former glacier dimensions; these markers, in conjunction with knowledge of the timing of their deposition, can be used to reconstruct glacier histories and extract key climate information 20 — Most alpine glaciers in the Northern Hemisphere reached their maximum Holocene extent sometime during the LIA, consistent with the long-term reduction in Northern Hemisphere insolation Thus, only moraines dating to the LIA or younger are typically preserved on the landscape, and consequently, directly dating these preserved moraines results in glacier histories that only span the past few hundred years.