Works matching IS 09212728 AND DT 2017 AND VI 58 AND IP 3
Results: 10
First evidence for the occurrence of Unapertura (Crustacea, Branchiopoda, Anomopoda, Chydoridae) in North America based on subfossil remains.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 291, doi. 10.1007/s10933-017-9978-7
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Lake evolution and hydroclimate variation at Lake Qinghai (China) over the past 32 ka inferred from ostracods and their stable isotope composition.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 299, doi. 10.1007/s10933-017-9979-6
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Climatic and limnological changes at Lake Karakul (Tajikistan) during the last ~29 cal ka.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 317, doi. 10.1007/s10933-017-9980-0
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Effects of long term nutrient and climate variability on subfossil Cladocera in a deep, subalpine lake (Lake Garda, northern Italy).
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 335, doi. 10.1007/s10933-017-9981-z
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An examination of the hypersaline phases of Eocene Lake Uinta, upper Green River Formation, Uinta Basin, Utah.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 353, doi. 10.1007/s10933-017-9983-x
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Paleolimnological features of a mega-lake phase in the Makgadikgadi Basin (Kalahari, Botswana) during Marine Isotope Stage 5 inferred from diatoms.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 373, doi. 10.1007/s10933-017-9984-9
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Sources of organic matter for bacteria in sediments of Lake Rotsee, Switzerland.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 391, doi. 10.1007/s10933-017-9985-8
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Aquatic macrophyte dynamics in Lake Karakul (Eastern Pamir) over the last 29 cal ka revealed by sedimentary ancient DNA and geochemical analyses of macrofossil remains.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 403, doi. 10.1007/s10933-017-9986-7
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Regional climate changes drive increased scaled-chrysophyte abundance in lakes downwind of Athabasca Oil Sands nitrogen emissions.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 419, doi. 10.1007/s10933-017-9987-6
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Response of Sandy Lake in Schirmacher Oasis, East Antarctica to the glacial-interglacial climate shift.
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- Journal of Paleolimnology, 2017, v. 58, n. 3, p. 275, doi. 10.1007/s10933-017-9977-8
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- Article