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• W4291109518 endingPage "111186" @default.
• W4291109518 startingPage "111186" @default.
• W4291109518 abstract "The Holocene vegetation in the Yangtze Delta is sensitive to global/regional climate change, sea-level oscillations, and human impacts, and it represents a valuable archive for deciphering environmental change. In this paper, the vegetation history of the northern Yangtze deltaic coast, and its response to climate/sea-level changes over the past 10.3 ka, have been investigated based on palynological assemblages from a well-dated sediment core (YZ07) in the northern Yangtze delta. Comparison of vegetation successions with regional climatic proxies, relative sea level change, and depositional environments suggests that this region was dominated by mixed subtropical and temperate forests in a warm /wet climate regime during the early Holocene (~10.3–8.7 ka), when it was characterized by tidally-influenced fluvial environments. From ~8.7 ka to 7.5 ka, subtropical and warm temperate pollen taxa decreased significantly while cool-tolerant conifers and grasses became more dominant, indicating a cooler and drier climate. During the mid-Holocene thermal optimum (~7.5–4.3 ka), mixed subtropical and temperate forests expanded markedly in coastal regions, caused by a return to a warm/wet climate during an episode of rising sea-level. At the start of late Holocene (~4.3 to 3.4 ka), subtropical and temperate trees were widely replaced by grasses around coastal environments, indicating a cooling climate. From ~3.4–1.7 ka, mixed subtropical and temperate forests flourished in the delta region, suggesting that climate returned to warm and wet conditions again. From ~1.7–1.3 ka, in delta environments, subtropical and temperate forests contracted under cool/dry climatic conditions. Since ~1.3 ka, subtropical and temperate pollen taxa increased around the marsh to intertidal flat environments, suggesting a warm/wet climate resurgence. The generally warm/wet Holoence climate of the Yangtze Delta region was interrupted by a series of short-term cold events at 8.2 ka, 7.3 ka, 4.2 ka, 3.5 ka and 1.4 ka. These fluctuations are broadly synchronous with regional climate variability and global sea-level oscillations. In addition, the influence of human cultivation on vegetation is recognized since the mid-Holocene (around 5.6 ka), with the appearance of Fagopyrum pollen in the northern Yangtze Delta." @default.
• W4291109518 created "2022-08-13" @default.
• W4291109518 creator A5000563498 @default.
• W4291109518 creator A5025936246 @default.
• W4291109518 creator A5039075009 @default.
• W4291109518 creator A5080841780 @default.
• W4291109518 date "2022-10-01" @default.
• W4291109518 modified "2023-09-27" @default.
• W4291109518 title "Palynology-based reconstruction of Holocene environmental history in the northern Yangtze Delta, China" @default.
• W4291109518 cites W1501181149 @default.
• W4291109518 cites W1951646693 @default.
• W4291109518 cites W1964609959 @default.
• W4291109518 cites W1974399951 @default.
• W4291109518 cites W1974755922 @default.
• W4291109518 cites W1975715178 @default.
• W4291109518 cites W1976989189 @default.
• W4291109518 cites W1978433101 @default.
• W4291109518 cites W1978712919 @default.
• W4291109518 cites W1982002336 @default.
• W4291109518 cites W1986443656 @default.
• W4291109518 cites W1990899433 @default.
• W4291109518 cites W1993257343 @default.
• W4291109518 cites W1994007098 @default.
• W4291109518 cites W1995047620 @default.
• W4291109518 cites W1995899017 @default.
• W4291109518 cites W1996932107 @default.
• W4291109518 cites W2002439403 @default.
• W4291109518 cites W2004864409 @default.
• W4291109518 cites W2007384214 @default.
• W4291109518 cites W2011696124 @default.
• W4291109518 cites W2013222518 @default.
• W4291109518 cites W2017548562 @default.
• W4291109518 cites W2018030672 @default.
• W4291109518 cites W2020023072 @default.
• W4291109518 cites W2020293415 @default.
• W4291109518 cites W2033021341 @default.
• W4291109518 cites W2036041264 @default.
• W4291109518 cites W2037732295 @default.
• W4291109518 cites W2040945899 @default.
• W4291109518 cites W2042032554 @default.
• W4291109518 cites W2042604187 @default.
• W4291109518 cites W2045026668 @default.
• W4291109518 cites W2045060693 @default.
• W4291109518 cites W2049686828 @default.
• W4291109518 cites W2050637326 @default.
• W4291109518 cites W2054303307 @default.
• W4291109518 cites W2054897620 @default.
• W4291109518 cites W2061303947 @default.
• W4291109518 cites W2061532387 @default.
• W4291109518 cites W2064759564 @default.
• W4291109518 cites W2068158963 @default.
• W4291109518 cites W2072573938 @default.
• W4291109518 cites W2076493751 @default.
• W4291109518 cites W2077280380 @default.
• W4291109518 cites W2080784268 @default.
• W4291109518 cites W2083662688 @default.
• W4291109518 cites W2083786328 @default.
• W4291109518 cites W2083897904 @default.
• W4291109518 cites W2084014771 @default.
• W4291109518 cites W2084413253 @default.
• W4291109518 cites W2086192317 @default.
• W4291109518 cites W2092234296 @default.
• W4291109518 cites W2092416196 @default.
• W4291109518 cites W2094350389 @default.
• W4291109518 cites W2101096368 @default.
• W4291109518 cites W2101307921 @default.
• W4291109518 cites W2103737089 @default.
• W4291109518 cites W2105583320 @default.
• W4291109518 cites W2111590126 @default.
• W4291109518 cites W2115594328 @default.
• W4291109518 cites W2124579984 @default.
• W4291109518 cites W2128349082 @default.
• W4291109518 cites W2129505768 @default.
• W4291109518 cites W2129616037 @default.
• W4291109518 cites W2137224021 @default.
• W4291109518 cites W2137645389 @default.
• W4291109518 cites W2140346246 @default.
• W4291109518 cites W2160579273 @default.
• W4291109518 cites W2161763833 @default.
• W4291109518 cites W2166451823 @default.
• W4291109518 cites W2168513163 @default.
• W4291109518 cites W2171607395 @default.
• W4291109518 cites W2208651932 @default.
• W4291109518 cites W2226015958 @default.
• W4291109518 cites W2279118301 @default.
• W4291109518 cites W2326032656 @default.
• W4291109518 cites W2336094506 @default.
• W4291109518 cites W2338939823 @default.
• W4291109518 cites W2414824932 @default.
• W4291109518 cites W2464339816 @default.
• W4291109518 cites W2528818077 @default.
• W4291109518 cites W2529808442 @default.
• W4291109518 cites W2548997294 @default.
• W4291109518 cites W2564434609 @default.
• W4291109518 cites W2578579055 @default.
• W4291109518 cites W2586922194 @default.
• W4291109518 cites W2594616905 @default.
• W4291109518 cites W2604523137 @default.

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