Lake Evolution in the Tengger Desert, Northwestern China, during the Last 40,000 Years
Dados Bibliográficos
| ID | 24088593 |
|---|---|
| Autores | Hans‐Joachim Pachur (Freie Universität Berlin), Hans-Joachim Pachur, Bernd Wünnemann (0000-0002-7172-735X, Freie Universität Berlin), Hucai Zhang (0000-0001-7733-2036, Lanzhou University of Technology) |
| Ano | 1995 |
| Volume | 44 |
| Fascículo | 2 |
| Páginas | 171-180 |
| Data de publicação | 1995-09-01 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | Quaternary Research (JOURNAL) |
| Identificadores do periódico | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Editora | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1006/qres.1995.1061 |
| OpenAlex | W2040399010 |
| Idioma | EN |
| Citações recebidas | 37 |
| Referências citadas | 14 |
Climatic changes inferred from lacustrine deposits and lake-level fluctuations in northwestern and central China are mainly based on paleoclimatic records from the Tibetan Plateau, while there is still a lack of data relating to the semiarid/arid desert regions of Inner Mongolia. In the Tengger Desert, different paleolake levels at Baijian Hu are documented by six paleoshorelines and stratified lake carbonates. The highest lake level occurred ca. 39,000 14 C yr B.P. and prevailed over about 16,000 km 2 . From sediment structure, geochemical composition, and ostracods we infer humid/cool conditions until 23,000 14 C yr B.P. In the northern Badanjilin Desert at Gaxan Nur/Sogu Nur, high lake levels can be deduced from mollusc-bearing paleobeaches and lake carbonates, which have been dated to 34,000 14 C yr B.P. and indicate a lake that covered some 32,000 km 2 . After ca. 20,000 yr B.P. the climate became dry with increased eolian activity and decreasing lake levels. Reestablishment of wet conditions occurred ca. 13,000 yr B.P. The Holocene is represented by stratified lake deposits that alternate with fluvial and eolian deposits, indicating a longterm oscillating trend toward arid conditions. The existence of widespread freshwater lakes during the late Pleistocene indicates a semihumid climate without an accompanying fall in temperature to arctic conditions.
Aeolian processes · Arctic · Arid · Climate change · Desert climate · Fluvial · Geography · Holocene · Hydrology (agriculture) · Paleoclimatology · Physical geography · Plateau (mathematics) · Pleistocene · Precipitation · Quaternary · Sediment · Structural basin · Coastal wetland ecosystem dynamics · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Oceanography · Paleontology
Surface exposure dating reveals MIS-3 glacial maximum in the Khangai Mountains of Mongolia
Hydrological and Climatic Changes in Deserts of China since the Late Pleistocene
Temperature variability and vertical vegetation belt shifts during the last ∼50,000 yr in the Qilian Mountains (NE margin of the Tibetan Plateau, China)
Tree-Ring δD as an Indicator of Asian Monsoon Intensity
A short chronology for the peopling of the Tibetan Plateau
Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years
The history and variability of the East Asian paleomonsoon climate
Late Pleistocene climate change and Paleolithic cultural evolution in northern China
The Loess/Paleosol record and the nature of the younger Dryas climate in central China
Hydrological changes and Holocene climate variations in NW China, inferred from lake sediments of Juyanze palaeolake by factor analyses
Late Pleistocene intensification technologies in Northern China
Oasis evolution processes and mechanisms in the lower reaches of Heihe River, Inner Mongolia, China since 1 ka ago
Holocene environmental changes in central Inner Mongolia revealed by luminescence dating of sediments from the Sala Us River valley
Holocene environmental change inferred from a high-resolution pollen record, Lake Zhuyeze, arid China
Past desertification processes of Minqin Oasis in arid China
Formation and paleoenvironment of rhizoliths of Shiyang River Basin, Tengeri Desert, NW China
Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (Western China and Western Mongolia)
Palaeodunes intercalated in loess strata from the western Chinese Loess Plateau
Formation and environmental significance of late Quaternary calcareous root tubes in the deserts of the Alashan Plateau, northwest China
The evolution of dry lands in northern China and in the Republic of Mongolia since the Last Glacial Maximum
Carbonate crusts of Paleolake Zhuyeze, Tengeri Desert, China
Spatial and temporal patterns of aeolian activities in the desert belt of northern China revealed by dune chronologies
Evolution of Luyang Lake since the last 34,000 years
Mid-Holocene Indian Summer Monsoon variability off the Andaman Islands, Bay of Bengal
A multi-proxy reconstruction of monsoon variability in the late Holocene, South India
Evolution of megadunes and lakes in the Badain Jaran Desert, Inner Mongolia, China during the last 31,000 years
Cultural responses to aridity in the Middle Holocene and increased social complexity
Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia
Lake evolution of the terminal area of Shiyang River drainage in arid China since the last glaciation
Geochemical evidence of the sources of aeolian sands and their transport pathways in the Minqin Oasis, northwestern China
Paleoenvironment of the Central Himalaya during late MIS 3 using stable isotopic compositions of lacustrine organic matter occluded in diatoms and sediments
Pleistocene paleoenvironmental changes in the high mountain ranges of central China and adjacent regions
Vegetation changes and associated climate variations during the past ∼38,000 years reconstructed from the Shaamar eolian-paleosol section, northern Mongolia
A Caveat on Radiocarbon Dating of Organic-Poor Bulk Lacustrine Sediments in Arid China
Dilemma of Dating on Lacustrine Deposits in an Hyperarid Inland Basin of NW China
Peopling of the northern Tibetan Plateau
Human Colonization of Asia in the Late Pleistocene
Paleoclimatic implications of late quaternary lacustrine sediments in Western Nubia, Sudan
Episode of Strengthened Summer Monsoon Climate of Younger Dryas Age on the Loess Plateau of Central China
Lacustrine Sedimentation in a Semiarid Alpine Setting
Lake evolution during the past 30,000 years in China, and its implications for environmental change
Lake Evolution during the Last 3000 Years in China and Its Implications for Environmental Change
Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years
A 13,000-year climate record from western Tibet
Vegetational and seasonal climatic changes since the last full glacial in the Thar Desert, northwestern India
Lake Qinghai, China
The climate of China
Paleoclimatic field studies in and along the Qinling Shan (Central China)
| Obras citantes distintas | 37 |
|---|---|
| Citações por ano | 1,32 |
| Intervalo de citações | 1998 - 2020 (23) |
| Velocidade de citação | historical |
| Altamente citado | Não |
| Tipos de citação | Neutras: 33 |