Age, Palaeoenvironments, and Climatic Significance of Late Pleistocene Konya Lake, Turkey
Bibliographic Data
| ID | 24087737 |
|---|---|
| Authors | Neil Roberts (0000-0001-5538-8653, Loughborough University, corresponding author) |
| Year | 1983 |
| Volume | 19 |
| Issue | 2 |
| Pages | 154-171 |
| Publication date | 1983-03-01 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Quaternary Research (JOURNAL) |
| Journal identifiers | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Publisher | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1016/0033-5894(83)90002-9 |
| OpenAlex | W2053377719 |
| Language | EN |
| Citations received | 30 |
| References cited | 22 |
The Konya Basin, a closed depression at the southern margin of the Anatolian Plateau, contained a shallow but extensive lake during the late Quaternary. Nearshore sands and gravels containing Dreissena shells form prominent depositional terraces around the basin edges at elevations between 1005 and 1020 m, and the highest has been dated at more than 30,000 yr B.P. The last major phase of limnic sedimentation occurred between 23,000 and 17,000 yr B.P., after which the lake fragmented into a number of subbasins or secondary depressions which evolved to become either marshes or playas. A final expansion of these residual lakes has been dated to ca. 11,000 yr B.P. in one secondary depression. Archaeological and other evidence indicate that only minor lake-level fluctuations occurred during the Holocene. The dominant sedimentary process over the last 10,000 years has been alluviation at the basin margin. The Konya sequence confirms that the most recent period of high-lake levels in the northern Near East was of the last glacial age. The palaeolakes of Anatolia and Iran were, however, more a product of reduced evaporation brought about by temperature depression than of changes in precipitation, and thus belie their often-used description as an indicator of “pluvial” climatic conditions.
Geography · Geomorphology · Glacial period · Holocene · Marsh · Period (music) · Physical geography · Plateau (mathematics) · Pleistocene · Pluvial · Quaternary · Sedimentary depositional environment · Sedimentary rock · Structural basin · Wetland · Archaeology and ancient environmental studies · Geology · Geology and Paleoclimatology Research · Marine and environmental studies · Paleontology
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Paleoclimatic and archeological implications of Pleistocene and Holocene environments in Azraq, Jordan
A late Pleistocene long pollen record from Lake Urmia, Nw Iran
Quantifying climatic change through the last glacial–interglacial transition based on lake isotope palaeohydrology from central Turkey
Comment on “Age, Palaeoenvironments, and Climatic Significance of Late Pleistocene Konya Lake, Turkey” by Neil Roberts
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Investigation of the Geological, Mineralogical, and Geochemical Contents of the Sedimentary Fills in the Northern Area of the Quaternary-Aged Bor Basin (Niğde/Turkey)
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Evironmental change in southwestern Iran
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The Palaeoecology of South Central Anatolia at the end of the Pleistocene and the beginning of the Holocene
Notes on Site Distribution in the Çumra Area
C Dating of Recent Crustal Movements in the Persian Gulf and Iranian Makran
| Unique citing works | 30 |
|---|---|
| Citations per year | 0,71 |
| Citation span | 1984 - 2027 (44) |
| Citation velocity | recent |
| Highly cited | No |
| Citation types | Neutral: 22 |