Mainstream migration events of the Yellow River and anthropogenic responses during the Mid-Holocene
Bibliographic Data
| ID | 14973229 |
|---|---|
| Authors | Tinglin Ru, Liwei Yang (0009-0008-7189-4482), Gesong Wei, Xinze Li (0000-0003-3513-209X), Zhanfang Hou (0000-0002-0691-3500), Yingying Chen (0000-0002-8772-5228), Shiyue Chen (0000-0003-1170-1948) |
| Year | 2024 |
| Volume | 685 |
| Pages | 14-23 |
| Publication date | 2024-03-01 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Quaternary International (JOURNAL) |
| Journal identifiers | ISSN: 1040-6182 • E-ISSN: 1873-4553 |
| Publisher | Elsevier BV (PUBLISHER) |
| DOI | 10.1016/j.quaint.2024.01.010 |
| OpenAlex | W4391466480 |
| Language | EN |
| Citations received | 1 |
| References cited | 24 |
Climate change · Environmental change · Flooding (psychology · Geography · Grassland · Holocene · Period (music · Physical geography · Vegetation (pathology · Geological formations and processes · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Ecology · Geology · Oceanography · Paleontology
Hydroclimatic changes in south-central China during the 4.2 ka event and their potential impacts on the development of Neolithic culture
Sea Level Change Through the Last Glacial Cycle
Flexible paleoclimate age-depth models using an autoregressive gamma process
Prehistoric and historic overbank floods in the Luoyang Basin along the Luohe River, middle Yellow River basin, China
Pollen record of precipitation changes during the Younger Dryas and Early Holocene in the North China Plain
Holocene palaeoflood events recorded by slackwater deposits along the Jin-shan Gorges of the middle Yellow River, China
Freshwater radiocarbon reservoir age in the lower Yellow River floodplain during the late Holocene
Palynological richness and evenness
Socio-economic Impacts on Flooding
The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)
| Citations per year | 1 |
|---|---|
| Citation span | 2026 - 2026 (1) |
| Highly cited | No |