Late Holocene pollen atlas of the Jiulongchi Wetland in the Fanjingshan National Nature Reserve, southwestern China

Review of Palaeobotany and Palynology, Journal Year: 2025, Volume and Issue: unknown, P. 105344 - 105344

Published: March 1, 2025

Language: Английский

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Oak pollen infrageneric classification-based winter temperature reconstruction since the marine isotope stage 5 in Southeast China

Palaeogeography Palaeoclimatology Palaeoecology, Journal Year: 2025, Volume and Issue: unknown, P. 112957 - 112957

Published: April 1, 2025

Language: Английский

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Human activities flexibility under volatile environment conditions around 4000 a BP: Insights from the Jinsha site in the Chengdu Plain, SW China

Quaternary Science Reviews, Journal Year: 2024, Volume and Issue: 326, P. 108501 - 108501

Published: Jan. 22, 2024

Language: Английский

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Modern pollen assemblages in lake surface sediments and their relationships with vegetation, climate, and human activities in Yunnan, SW China

Review of Palaeobotany and Palynology, Journal Year: 2024, Volume and Issue: unknown, P. 105205 - 105205

Published: Sept. 1, 2024

Language: Английский

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Vegetation Dynamics since the Last Glacial Maximum in Central Yunnan, Southwest China

Forests, Journal Year: 2024, Volume and Issue: 15(7), P. 1075 - 1075

Published: June 21, 2024

Vegetation dynamics data since the Last Glacial Maximum (LGM) are essential for our understanding of ecosystem shifts and vegetation responses to climate change. Here, we present a pollen record covering last 25,000 years from Lake Fuxian in central Yunnan, southwest China. Our study shows seven stages LGM: The early LGM (stage 7 25,000–21,200 cal. BP) witnessed less dense regional dominated by pine forests, evergreen broadleaved forests (EBFs), deciduous (DBFs), montane hemlock fir/spruce forests. late 6 21,200–17,500 saw an expansion grasslands, wetlands, as well shrinkage EBFs DBFs. During deglaciation 5 17,500–13,300 BP), was oak alder densest occurred stage 4 13,300–11,200 BP, roughly equal Younger Dryas Chron, when DBFs, EBFs, wetlands grew catchment. mid-Holocene 3 11,200–5000 sweetgum addition some EBFs. After 5000 density became lower lower, thinner thinner. Pine expanded their maximum entire sequence 2 5000–2500 BP. A big deforestation event 1 (the 2500 years), cultivated catchment Fuxian. also experienced six major transitions, five centennial shift events, one large-scale long-term event. These resulted changes during LGM, deglaciation, early–mid-Holocene, human influence Holocene. has changed with 25° N summer insolation.

Language: Английский

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Pollen atlas and morphological analysis of the selected types from southeastern Tibet, China

Review of Palaeobotany and Palynology, Journal Year: 2024, Volume and Issue: 332, P. 105188 - 105188

Published: Sept. 3, 2024

Language: Английский

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Environmental changes and human impacts over the past 1200 years: Evidence from high-resolution pollen records from peat in the Yunnan-Guizhou Plateau, Southwest China

Palaeogeography Palaeoclimatology Palaeoecology, Journal Year: 2024, Volume and Issue: unknown, P. 112540 - 112540

Published: Oct. 1, 2024

Language: Английский

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Relative sea-level reconstructions by using foraminiferal transfer functions

Marine Micropaleontology, Journal Year: 2024, Volume and Issue: 192, P. 102410 - 102410

Published: Sept. 1, 2024

Language: Английский

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New quantified climate reconstruction in southern China suggests a potential influence of winter cloud cover across East Asia during the Holocene

The Science of The Total Environment, Journal Year: 2024, Volume and Issue: 958, P. 178008 - 178008

Published: Dec. 10, 2024

Language: Английский

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Unraveling the early human impacts on the ecosystem of Dianchi Lake: A 20,000-year diatom record from the southeastern Tibetan Plateau

Quaternary Science Reviews, Journal Year: 2024, Volume and Issue: 337, P. 108813 - 108813

Published: July 5, 2024

Language: Английский

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