Synonymer & Anagram | Engelska ordet LGM

Exempel på hur man kan använda LGM i en mening

• This wave of anatomically modern humans includes fossils of the Ahmarian, Bohunician, Aurignacian, Gravettian, Solutrean and Magdalenian cultures, extending throughout the Last Glacial Maximum (LGM), covering the period of roughly 48,000 to 15,000 years ago.
• Genetic studies indicate that the Magdalenian peoples were largely descended from earlier Western European Cro-Magnon groups like the Gravettians that were present in Western Europe over 30,000 years ago prior to the Last Glacial Maximum, who had retreated to southwestern Europe during the LGM.
• In Western Eurasia, the Paleolithic eases into the so-called Epipaleolithic or Mesolithic from the end of the LGM, beginning 15 ka.
• In the Hex River Mountains, in the Western Cape, block streams and terraces found near the summit of Matroosberg evidences past periglacial activity which likely occurred during the LGM.
• This technique has been used to quantify the Atlantic Meridional Overturning Circulation (AMOC) during the Last Glacial Maximum (LGM) and during abrupt climate change events in Earth's past, such as Heinrich events and Dansgaard-Oeschger events.
• T2c and T2d appear to have a Near Eastern origin around the time of the Last Glacial Maximum (LGM) and more recent dispersals into Europe.
• By the end of the LGM, after 20 ka, A Western European lineage, dubbed west European hunter-gatherer (WHG) emerged from the Solutrean refugium during the European Mesolithic.
• The deep oceans were depleted in radiocarbon during the deglaciation following the LGM, which has been hypothesised to be the result of sluggish meridional overturning circulation or due to a release of volcanic carbon or methane clathrates into abyssal waters.
• Modern humans recolonize territories lost during the Last Glacial Maximum (LGM) and push into northern Europe for the first time, coming from the comparatively warmer Franco-Cantabrian region, where the Magdalenian originated.
• The Gravettian split into the Epi-Gravettian in the east and Solutrean in the west, due to major climatic degradation during the Last Glacial Maximum (LGM), peaking 21,000 years ago.
• The three main lobes of the Fennoscandian Ice Sheet in Russia during the LGM followed the basins of Rybinsk and the rivers of Dvina, Vologda.
• Røed, using gel electrophoresis to analyze genetic variation in Svalbard reindeer compared to wild Norwegian reindeer, reported "unique alleles in the loci coding for transferrin and acid phosphatase for the two subspecies indicate that there has been no interbreeding in recent time" and estimated divergence 225,000 years ago, that is, during the interstadial before the last glacial maximum (LGM).
• During the Last Glacial Maximum (LGM), approximately 20,000 years ago, a valley glacier carved the Carbajal-Tierra Mayor valley (described as the "glaciation axis of the Fuegian Andes") from northwest to southeast, with an ice tongue forking south along the Valle Río Olivia into the Beagle Channel immediately to the east of Ushuaia.
• The region of modern-day Croatia was part of a wider Balkan region which may have served as one of several refugia during the LGM, a source region for the recolonization of Europe during the post-glacial period and Holocene (10,000 years ago).
• estimate an isolation period in Beringia of about ≈10,000 years, concluding that the isolated Beringian populations spread throughout mid-latitude and South America after the LGM due to blocked access to North America before 15,000 cal BP.
• During the dramatic landscape transition occurring throughout Beringia from the Pleistocene LGM into the early Holocene the arid tundra was replaced as shrubs expanded in warmer and wetter periods, eventually creating the mosaic of peatlands, boreal forest, and thaw lakes that characterizes the region today.
• Early Lake Estancia, most likely larger than the LGM lake, existed possibly during the Illinoian glaciation and largely dried up in the warm and dry climate of the Sangamonian interglacial.

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