about
A high-performance, safer and semi-automated approach for the delta18O analysis of diatom silica and new methods for removing exchangeable oxygen.The seasonal sea-ice zone in the glacial Southern Ocean as a carbon sinkComparison of water isotope-ratio determinations using two cavity ring-down instruments and classical mass spectrometry in continuous ice-core analysis.Combined approach of isotope mass balance and hydrological water balance methods to constrain the sources of lake water as exemplified on the small dimictic lake Silbersee, northern Germany.Corrigendum: The seasonal sea-ice zone in the glacial Southern Ocean as a carbon sink.The deuterium excess records of EPICA Dome C and Dronning Maud Land ice cores (East Antarctica)Late Quaternary vegetation and lake system dynamics in north-eastern Siberia: Implications for seasonal climate variabilityHolocene environment of Central Kamchatka, Russia: Implications from a multi-proxy record of Two-Yurts LakeHolocene freshwater diatoms: palaeoenvironmental implications from south Kamchatka, RussiaOxygen isotope composition of diatoms as Late Holocene climate proxy at Two-Yurts Lake, Central Kamchatka, RussiaLate Holocene diatom assemblages in a lake-sediment core from Central Kamchatka, RussiaPalaeoclimate signals as inferred from stable-isotope composition of ground ice in the Verkhoyansk foreland, Central YakutiaIce Complex permafrost of MIS5 age in the Dmitry Laptev Strait coastal region (East Siberian Arctic)Dissolved organic carbon (DOC) in Arctic ground iceEstimation and calibration of the water isotope differential diffusion length in ice core recordsConstraints on post-depositional isotope modifications in East Antarctic firn from analysing temporal changes of isotope profilesOxygen and carbon isotope composition of modern planktic foraminifera and near-surface waters in the Fram Strait (Arctic Ocean) – a case studyRegional climate signal vs. local noise: a two-dimensional view of water isotopes in Antarctic firn at Kohnen Station, Dronning Maud LandA 250 ka oxygen isotope record from diatoms at Lake El'gygytgyn, far east Russian ArcticIce wedges as archives of winter paleoclimate: A reviewGround-ice stable isotopes and cryostratigraphy reflect late Quaternary palaeoclimate in the Northeast Siberian Arctic (Oyogos Yar coast, Dmitry Laptev Strait)Northeast Siberian ice wedges confirm Arctic winter warming over the past two millenniaLong-term winter warming trend in the Siberian Arctic during the mid- to late HoloceneIce Complex formation in arctic East Siberia during the MIS3 InterstadialEurasian Arctic climate over the past millennium as recorded in the Akademii Nauk ice core (Severnaya Zemlya)Last Glacial Maximum records in permafrost of the East Siberian ArcticPalaeoclimatic information from stable water isotopes of Holocene ice wedges on the Dmitrii Laptev Strait, northeast Siberia, RussiaLateglacial and Holocene isotopic and environmental history of northern coastal Alaska – Results from a buried ice-wedge system at BarrowPermafrost evidence for severe winter cooling during the Younger Dryas in northern Alaska115 year ice-core data from Akademii Nauk ice cap, Severnaya Zemlya: high-resolution record of Eurasian Arctic climate changeA 275 year ice-core record from Akademii Nauk ice cap, Severnaya Zemlya, Russian ArcticEastern Beringia and beyond: Late Wisconsinan and Holocene landscape dynamics along the Yukon Coastal Plain, CanadaModern and Late Holocene Retrogressive Thaw Slump Activity on the Yukon Coastal Plain and Herschel Island, Yukon Territory, CanadaOrigin and characteristics of massive ground ice on Herschel Island (western Canadian Arctic) as revealed by stable water isotope and Hydrochemical signaturesLate Quaternary paleoenvironmental records from the Chatanika River valley near Fairbanks (Alaska)Inter-laboratory comparison of oxygen isotope compositions from biogenic silicaLake nutrient variability inferred from elemental (C, N, S) and isotopic (δ13C, δ15N) analyses of aquatic plant macrofossilsThe mystery of Bunge Land (New Siberian Archipelago): implications for its formation based on palaeoenvironmental records, geomorphology, and remote sensingUsing variations in the stable carbon isotope composition of macrophyte remains to quantify nutrient dynamics in lakesEvaporation effects as reflected in freshwaters and ostracod calcite from modern environments in Central and Northeast Yakutia (East Siberia, Russia)
P50
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P50
description
forsker
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հետազոտող
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name
H. Meyer
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H. Meyer
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H. Meyer
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Hanno Meyer
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Hanno Meyer
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Hanno Meyer
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H. Meyer
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H. Meyer
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H. Meyer
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Hanno Meyer
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Hanno Meyer
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H. Meyer
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H. Meyer
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H. Meyer
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Hanno Meyer
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Hanno Meyer
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Hanno Meyer
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P214
P227
P244
P1153
7404226510
P213
0000 0001 1626 3161
P214
P227
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nb2004015237
P31
P496
0000-0003-4129-4706
P569
1969-01-01T00:00:00Z
P734
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lccn-nb2004015237