This paper presents the results of a dual approach for assessing fossil benthic foraminiferal communities using both traditional morphology‐based analyses and sedimentary ancient DNA (sedaDNA) metabarcoding. The main objectives are to test the feasibility of sedaDNA analyses to assess foraminiferal biodiversity in temperate shelf sediments (Le Croisic,
Meryem Mojtahid+13 more
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Crevasse density, orientation and temporal variability at Narsap Sermia, Greenland. [PDF]
Van Wyk de Vries M, Lea JM, Ashmore DW.
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Neoglacial and historical glacier changes around Kangersuneq fjord in southern West Greenland [PDF]
The Nuup Kangerlua region in southern West Greenland became eglaciated in the early Holocene and by the mid-Holocene, the margin of the Inland Ice was located east of its present position.
Weidick, Anker+3 more
doaj
Clast‐fabric analysis is a widely used method for investigating depositional and deformation processes in glacial sediments. However, traditional field‐based approaches lack standardization, are time consuming and introduce sampling bias. This study aimed to develop a novel approach to automate clast‐fabric analysis using machine learning‐based image ...
Bennet Schuster+7 more
wiley +1 more source
Geoffrey S. Hope and others, ed. The equatorial glaciers of New Guinea. Results of the 1971-1973 Australian universities’ expeditions to Irian Jaya: survey, glaciology, meteorology, biology and palaeo-environments, edited by Geoffrey S. Hope, James A. Peterson, Uwe Radok, Ian Allison. Rotterdam , A. A. Balkema, 1976. xii, 244p. Guilders 39.50. [PDF]
R. G. Barry
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Quaternary glaciation history and glaciology of Jakobshavn Isbræ and the Disko Bugt region, [PDF]
The Disko Bugt region in central West Greenland is characterised by permanent ice streams, of which Jakobshavn Isbræ is by far the most important. The first thorough studies on the glaciology of the region were conducted over 150 years ago by H.J.
Bennike, Ole, Weidick, Anker
doaj
Shoreline and deglaciation chronology in southeast Norway
The postglacial relative sea level history is reconstructed in four areas of mid‐ and inner Oslofjorden in southeast Norway. The reconstructions are based on radiocarbon‐dated raised shoreline levels from 42 sites, mainly isolation basins, and limiting ages from four lakes above the marine limit.
Anders Romundset+6 more
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Address of Welcome to the Participants in the Third International Symposium on Antarctic Glaciology [PDF]
Edward H. Jennings
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High‐resolution LiDAR data with field validation of inferred southern Ontario ice stream terrains indicate that steady‐state ice streaming is difficult to reconcile with our observations. Rather, these new observations show strong evidence of significant fluvial scouring across the area in which meltwater sheet flow overtopped the landscape.
David R. Sharpe, Chris C. Smart
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Remote Sensing Application in Mountainous Environments: A Bibliographic Analysis. [PDF]
Jombo S+3 more
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