Stalagmite evidence of Last Glacial Maximum to early Holocene climate variability in southwestern Iran
Author:
Affiliation:
1. Institute of Geology University of Innsbruck Innsbruck Austria
2. Department of Geology University of Isfahan Isfahan Iran
3. Department of Earth Sciences University of Cambridge Cambridge UK
Publisher
Wiley
Subject
Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3478
Reference72 articles.
1. Climatic variability during the last ∼90ka of the southern and northern Levantine Basin as evident from marine records and speleothems
2. Late glacial and early Holocene hydroclimate variability in northwest Iran (Talesh Mountains) inferred from chironomid and pollen analysis
3. A major hydrobiological change in Dasht-e Arjan Wetland (southwestern Iran) during the late glacial – early Holocene transition revealed by subfossil chironomids
4. Testing Theoretically Predicted Stalagmite Growth Rate with Recent Annually Laminated Samples: Implications for Past Stalagmite Deposition
5. Sea–land oxygen isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implication for paleorainfall during interglacial intervals
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1. Decoupled Hydroclimate of Central and Southwestern Iran Controlled by the Strength of Southerly‐Westerly Jets During Marine Isotope Stage 3;Geophysical Research Letters;2024-06-27
2. Sedimentary evolution and lake level fluctuations of Urmia Lake (north‐west Iran) over the past 50 000 years; insights from Artemia faecal pellet records;Sedimentology;2023-11-29
3. Vegetation and climate dynamics at the dawn of human settlement: multiproxy palaeoenvironmental evidence from the Hashilan Wetland, western Iran;Journal of Quaternary Science;2023-07-21
4. High-resolution record of stable isotopes in soil carbonates reveals environmental dynamics in an arid region (central Iran) during the last 32 ka;Frontiers in Earth Science;2023-05-25
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