Implications of submonthly oxygen and carbon isotope variations in late Pleistocene Melanopsis shells for regional and local hydroclimate in the upper Jordan River valley
Datos Bibliográficos
| ID | 24088500 |
|---|---|
| Autores | Addison Rice (0000-0002-4507-6717, University of Iceland, autor de correspondencia), Elizabeth Bunin (0000-0001-8108-2746, University of Iceland), Birgit Plessen (GFZ Helmholtz Centre for Geosciences), Gonen Sharon (0000-0002-1226-2556, Tel Hai Academic College), Steffen Mischke (0000-0003-3821-8497, University of Iceland) |
| Año | 2023 |
| Volumen | 115 |
| Páginas | 146-159 |
| Fecha de publicación | 2023-09-01 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Quaternary Research (JOURNAL) |
| Identificadores de la revista | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Editorial | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1017/qua.2023.25 |
| OpenAlex | W4381376886 |
| Idioma | EN |
| Citas recibidas | 2 |
| Referencias citadas | 71 |
Many water-stressed regions of the globe have a highly seasonal precipitation regime. However, seasonality in the past and under changing climates is little studied. Submonthly records of sclerochronological δ 18 O and δ 13 C values of Melanopsis shells from the Jordan River Dureijat archaeological site (JRD) in the upper Jordan River valley presented here document the hydrology of paleo-Lake Hula. These records were assessed for changes in seasonal hydrology in the lake and compared with modern shells collected from present-day waterbodies in northern Israel and with models of δ 18 O shell . Results from shells in sediments dating from the last glacial maximum (LGM) to the Bølling-Allerød imply changes in waterbody size that qualitatively parallel changes in the late Pleistocene Lake Lisan levels; Hula Lake was well buffered when Lake Lisan stood at a high stand and poorly buffered when water levels were lower. Furthermore, data from shells dated to the LGM suggest inflowing water with lower δ 18 O values than local rainfall, providing evidence for a greater proportion of snow in the catchment than today. Reconstruction of water δ 18 O and mixing-model calculations suggest that snowmelt contribution to spring water during the LGM may have been more than twice the amount in the modern-day catchment.
Discharge · Drainage basin · Geochemistry · Geography · Geomorphology · Glacial period · Hydrology (agriculture) · Isotopes of oxygen · Last Glacial Maximum · Physical geography · Pleistocene · Precipitation · Snow · Snowmelt · Spring (device) · Geology · Geology and Paleoclimatology Research · Groundwater and Isotope Geochemistry · Paleontology
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| Obras citantes distintas | 2 |
|---|---|
| Citas por año | 1 |
| Intervalo de citas | 2024 - 2026 (3) |
| Velocidad de citación | current |
| Altamente citado | No |
| Tipos de cita | Neutras: 2 |