about
Western Mediterranean hydro-climatic consequences of Holocene iceberg advances (Bond events)Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum – extending the concept of pollen source area to pollen-based climate reconstructions from large lakesHolocene lake stages and thermokarst dynamics in a discontinuous permafrost affected region, north-eastern Tibetan PlateauEcological development of Lake Donggi Cona, north-eastern Tibetan Plateau, since the late glacial on basis of organic geochemical proxies and non-pollen palynomorphsLate Glacial and Holocene development of Lake Donggi Cona, north-eastern Tibetan Plateau, inferred from sedimentological analysisBasin morphology and seismic stratigraphy of Lake Donggi Cona, north-eastern Tibetan Plateau, ChinaOstracods and stable isotopes of a late glacial and Holocene lake record from the NE Tibetan PlateauQuantitative relationship between water-depth and sub-fossil ostracod assemblages in Lake Donggi Cona, Qinghai Province, ChinaModern hydrology and late Holocene history of Lake Karakul, eastern Pamirs (Tajikistan): A reconnaissance studyLate Quaternary environments in the Gobi Desert of Mongolia: Vegetation, hydrological, and palaeoclimate evolutionClimate variability on the south-eastern Tibetan Plateau since the Lateglacial based on a multiproxy approach from Lake Naleng – comparing pollen and non-pollen signalsA modern pollen-climate calibration set from central-western Mongolia and its application to a late glacial-Holocene recordMoisture-advection feedback supports strong early-to-mid Holocene monsoon climate on the eastern Tibetan Plateau as inferred from a pollen-based reconstructionRecent ecological responses to climate variability and human impacts in the Nianbaoyeze Mountains (eastern Tibetan Plateau) inferred from pollen, diatom and tree-ring dataWhat drives the recent intensified vegetation degradation in Mongolia – Climate change or human activity?Environmental variability in the monsoon–westerlies transition zone during the last 1200 years: lake sediment analyses from central Mongolia and supra–regional synthesisEnvironmental constraints on lake sediment mineral compositions from the Tibetan Plateau and implications for paleoenvironment reconstructionSubfossil ostracode assemblages from Mongolia – Quantifying response for paleolimnological applicationsModest diatom responses to regional warming on the southeast Tibetan Plateau during the last two centuriesReconstructing climate variability on the northeastern Tibetan Plateau since the last Lateglacial – a multi-proxy, dual-site approach comparing terrestrial and aquatic signalsTerrestrial and aquatic responses to climate change and human impact on the southeastern Tibetan Plateau during the past two centuriesA modern pollen-climate calibration set based on lake sediments from the Tibetan Plateau and its application to a Late Quaternary pollen record from the Qilian MountainsAn ostracod-inferred large Middle Pleistocene freshwater lake in the presently hyper-arid Qaidam Basin (NW China)Biomarker and compound-specific δ13C evidence for changing environmental conditions and carbon limitation at Lake Koucha, eastern Tibetan PlateauHolocene treeline shifts and monsoon variability in the Hengduan Mountains (southeastern Tibetan Plateau), implications from palynological investigationsLake nutrient variability inferred from elemental (C, N, S) and isotopic (δ13C, δ15N) analyses of aquatic plant macrofossilsLate Quaternary environmental history of the south-eastern Tibetan Plateau inferred from the Lake Naleng non-pollen palynomorph recordLate glacial vegetation and climate oscillations on the southeastern Tibetan Plateau inferred from the Lake Naleng pollen profileLateglacial and Holocene variation in aeolian sediment flux over the northeastern Tibetan Plateau recorded by laminated sediments of a saline meromictic lakeUsing variations in the stable carbon isotope composition of macrophyte remains to quantify nutrient dynamics in lakesQuantitative climate and vegetation trends since the late glacial on the northeastern Tibetan Plateau deduced from Koucha Lake pollen spectraReduced early Holocene moisture availability in the Bayan Har Mountains, northeastern Tibetan Plateau, inferred from a multi-proxy lake recordAn ostracod-conductivity transfer function for Tibetan lakesTemperature variability and vertical vegetation belt shifts during the last ∼50,000 yr in the Qilian Mountains (NE margin of the Tibetan Plateau, China)A Late Quaternary lake record from the Qilian Mountains (NW China): lake level and salinity changes inferred from sediment properties and ostracod assemblagesA late Quaternary lake record from the Qilian Mountains (NW China): evolution of the primary production and the water depth reconstructed from macrofossil, pollen, biomarker, and isotope dataSub-Recent Ostracoda from Qilian Mountains (NW China) and their ecological significanceSedimentary record of coseismic subsidence in Hersek coastal lagoon (Izmit Bay, Turkey) and the late Holocene activity of the North Anatolian FaultVegetation change in the eastern Pamir Mountains, Tajikistan, inferred from Lake Karakul pollen spectra of the last 28 kyrAn expanded ostracod-based conductivity transfer function for climate reconstruction in the Levant
P50
Q56251970-DC5033E1-CBE0-4C4A-A205-13C45B66B850Q57494348-08E283DC-B36A-48C2-BDEF-50A6AE7486E1Q57494376-AD23D94C-990E-4562-B27C-3474A41663A9Q57494413-172FEE8F-93B1-432C-BA98-43EE63F25F4DQ57494421-C2D9D699-2A84-4D5F-999D-BC134591B839Q57494442-5BC9CEE9-1842-48D8-AAE7-26DD6E7220EEQ57494450-95078794-4207-4A6F-A0A0-62C752442251Q57494453-AE8689E5-49A4-4EEB-818B-235AF796EA57Q57538025-105FD023-B0A5-40CF-8DD6-E2A8325BCF15Q57836950-F46C7B00-3DD1-4035-971C-F31B67608750Q58086091-FB199B97-94AE-42C9-A720-071B083A01D9Q58086126-56BF158B-9721-4C27-A01E-37F5D5B4885FQ58086152-5C21ACC9-FA14-48AC-A18B-20BE4067BBDEQ58086160-43709199-16C7-494F-BA96-D16648E49FB0Q58086173-71010BCC-CA87-43B2-881B-A307C2DAF0B6Q58086190-484340F3-2868-4AE6-872C-2CD55942EC48Q58086224-B92A61B0-630B-48E5-846E-0C5F3BBBCBA6Q58086240-ADC82AF4-7EC6-4BE9-9F1E-FB94EC8E28CDQ58086264-1C2091B6-0341-4AA9-822A-30307CFFC4E7Q58086277-75C88C26-E15C-4FB2-9D00-A284ACDC06ECQ58086284-9E8E5CC6-751D-4ACF-934A-8D7AC399B04BQ58086287-9A3E1541-E832-4D68-8E10-284253B26557Q58086289-E08080DB-AAEE-4D26-803F-ED3BB90917DCQ58086295-3F44A018-59D7-483D-BE7D-4B03F7DEA9E7Q58086305-30913022-5658-4463-80EF-9090C5763ABBQ58086312-AD115938-AC8C-4D9F-BA54-860E40DB0D1CQ58086316-A4979060-15E6-4FDA-A351-0A6EDB6C9F1AQ58086321-F1D10D55-585E-46B5-9DA0-4BFB515C7148Q58086325-785C0AB7-5A27-4883-BF73-A98DB33CE7E9Q58086343-99519DE7-7E7A-4DF3-A14B-A2FBA570CB91Q58086361-58A089F6-DEDB-474D-8100-980656A63A7AQ58086372-55E7200F-82E6-4E1F-B010-1B16D9EF0F55Q58086376-CD49D16D-5401-4051-9A8C-A2EB6420E28FQ58086401-90BD6D83-BCF8-4C45-A8EE-B9666FC01784Q58086404-141DB73D-2890-49F9-AEBA-0741AF1B074BQ58086407-394CF93A-1578-4C02-8B6F-5B0F250FC8C7Q58086417-45C33EBB-4DDB-462D-91E9-0ED49D09AF03Q59847223-5C242BA5-2401-49DC-BEDB-97A8DD1E7531Q60546022-B3428A65-B7C9-402C-9404-2DA4F020FD8DQ62564602-9762B87B-0783-49AE-8AA9-49E804EE41C8
P50
description
researcher
@en
ricercatore
@it
wetenschapper
@nl
հետազոտող
@hy
name
Steffen Mischke
@ast
Steffen Mischke
@en
Steffen Mischke
@es
Steffen Mischke
@nl
type
label
Steffen Mischke
@ast
Steffen Mischke
@en
Steffen Mischke
@es
Steffen Mischke
@nl
prefLabel
Steffen Mischke
@ast
Steffen Mischke
@en
Steffen Mischke
@es
Steffen Mischke
@nl
P227
P21
P214
337153472504845360000
P227
1164780077
P31
P496
0000-0003-3821-8497
P7859
viaf-337153472504845360000