The Yangtze River Delta experienced strong seasonality and regular summer upwelling during the warm mid-Holocene
Abstract The mid-Holocene climate optimum saw warm temperatures in large parts of China, but its impact on seasonal environmental changes is not fully understood yet. Here, we use high-resolution geochemical analyses of 7000 to 6000 year-old oyster shells from the Yangtze River Delta to reconstruct...
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Published in | Communications earth & environment Vol. 5; no. 1; pp. 492 - 10 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
London
Nature Publishing Group
08.09.2024
Nature Portfolio |
Subjects | |
Online Access | Get full text |
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