Titlebook: Limnogeology: Progress, Challenges and Opportunities; A Tribute to Elizabe Michael R. Rosen,David B. Finkelstein,Sila Pla-Pue Book 2021 The

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Modern and Ancient Animal Traces in the Extreme Environments of Lake Magadi and Nasikie Engida, Kenynt inflow from hot springs and magmatic CO., producing high-carbonate-bicarbonate, high-sodium waters with little calcium in a semi-arid closed lake basin. Hypersalinity, hyperalkalinity, and hydrothermal conditions characterize the modern lake and lake margins, and also contributed to the environme

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Barrister

How Changes of Past Vegetation and Human Impact Are Documented in Lake Sediments: Paleoenvironmentalcal questions about settlement and land use history in Central Europe. The primary aim was to establish well-dated pollen profiles with very high temporal resolution. A major focus was to reconstruct the extent and intensity of land clearing during the Neolithic, the Iron Age, the Roman Period as we

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Large-Scale Slumps and Associated Resedimented Deposits in Miocene Lake Basins from SE Spainuccession of the Cenajo and Las Minas Basins. The basins display half-graben geometries where the northern margins consist of a network of large and deep, listric normal faults. The largest single deformational unit, reaching up 40 m in thickness, crops out in the Cenajo Basin and consists of soft-s

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Lacustrine and Fluvial Carbonate Microbialites in the Neogene of the Ebro Basin, Spain: A Summary ofhe Sierra de Alcubierre and Montes de Castejón) and fluvial to fluvio-lacustrine environments (middle to upper Miocene in the Muela de Borja and Montolar hill), in the Ebro Basin. Saline and freshwater conditions were deduced from sedimentological features and stable isotope composition (δ.C and δ.O

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Ecological Response of Ostracodes (Arthropoda, Crustacea) to Lake-Level Fluctuations in the Eocene Gum (EECO). Two species of ostracodes, . (Swain, Journal of Paleontology, 23:172–181, 1949) and . (Swain, Journal of Paleontology, 23:172–181, 1949), were recovered from 16 intervals at three sites from Fossil Basin, Wyoming, USA. Population density per sample was quantified as the number of ostracod

平淡而無味

History of Great Salt Lake, Utah, USA: since the Termination of Lake Bonneville ideas and essential data. The published literature, however, can be confusing and misleading. In this chapter, we review and provide context for a number of those publications. This chapter is intended as a summary of what is known, what is not known, and what cannot be known with precision about t

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What’s New About the Old Bonneville Basin? Fresh Insights About the Modern Limnogeology of Great Saleville, and today is the fourth largest perennial and closed basin lake in the world. More than a century of study on the Pleistocene megalake and its modern hypersaline environment (latitude 40.7° to 41.7°N, longitude 111.9° to 113.1°W) has significantly contributed to what we know about lake syste

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Middle Holocene Hydrologic Changes Catalyzed by River Avulsion in Big Soda Lake, Nevada, USAe surrounding aquifer and the only surface water input is rainfall, which is negligible. A core taken in 2010 records an 8.75 m depositional history of the lake. A radiocarbon date on fossil pollen from 8.4 m below the sediment water interface (BSWI) of 14,740 (+1120/?825) cal?yr BP suggests that th

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