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- W4293090451 abstract "Summary The Late Triassic Fleming Fjord Group of the Jameson Land Basin in central East Greenland constitutes a 350 m thick succession of well-exposed lake sediments. The lake succession has been dated by magnetostratigraphy to the Norian (220 -209 Ma). The depositional system is composed of four lake units: shallow-lake sediments with dolostones and stromatolitic limestones, ephemeral lake and mudflat deposits dominated by sandy facies, ephemeral lake and mudflat deposits dominated by muddy facies, and ephemeral to perennial lake deposits with common dolomitic marlstone facies. The two middle units form a red bed succession with common bone remains of dinosaurs. All lake units display composite cyclicity, which is believed to record orbital control on precipitation, sediment load to the basin, and depositional processes in the basin. Precession, obliquity and eccentricity cycles can be identified including the long eccentricity cycle of 405 kyr. The lake basin was situated at the norther rim of Panagaea at 43° N most likely in a semi-humid to humid climate belt influenced by westerlies. The basin experienced a northward drift of about 6 degrees during its life span. This is believed to have changed the overall climate and thereby caused the observed evolution of the lake system." @default.
- W4293090451 created "2022-08-26" @default.
- W4293090451 creator A5010354162 @default.
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- W4293090451 date "2021-01-01" @default.
- W4293090451 modified "2023-09-30" @default.
- W4293090451 title "A 10-Myr record of Late Triassic lake deposition, Fleming Fjord Group, East Greenland" @default.
- W4293090451 doi "https://doi.org/10.3997/2214-4609.202112761" @default.
- W4293090451 hasPublicationYear "2021" @default.
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