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Hydrological sensitivity and carbon dynamics during the evolution of a crater lake peatland in Northeast China
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DOI：10.1016/j.catena.2026.110486.png)
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Abstract
En 中文
• Peat initiation was asynchronous across the crater lake, modulated by basal topography and climate. • Crater lake water-level shifts reveal decoupled temperature and monsoon controls across timescales. • Holocene carbon accumulation phased differences driven by water-level changes and vegetation. • MWP and LIA had similar carbon accumulation from distinct productivity–decomposition balances. • Recent carbon accumulation surge exceeds climate effects, implicating drainage and volcanic inputs.
Keywords:
Peatland
Paludification
Carbon accumulation
Plant macrofossils
Water-level reconstruction
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5.7
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9.2K
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