Short communication: Massive erosion in monsoonal central India linked to late Holocene land cover degradation


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Date

2017

Publication Type

Journal Article

ETH Bibliography

yes

Citations

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Data

Abstract

Soil erosion plays a crucial role in transferring sediment and carbon from land to sea, yet little is known about the rhythm and rates of soil erosion prior to the most recent few centuries. Here we reconstruct a Holocene erosional history from central India, as integrated by the Godavari River in a sediment core from the Bay of Bengal. We quantify terrigenous fluxes, fingerprint sources for the lithogenic fraction and assess the age of the exported terrigenous carbon. Taken together, our data show that the monsoon decline in the late Holocene significantly increased soil erosion and the age of exported organic carbon. This acceleration of natural erosion was later exacerbated by the Neolithic adoption and Iron Age extensification of agriculture on the Deccan Plateau. Despite a constantly elevated sea level since the middle Holocene, this erosion acceleration led to a rapid growth of the continental margin. We conclude that in monsoon conditions aridity boosts rather than suppresses sediment and carbon export, acting as a monsoon erosional pump modulated by land cover conditions.

Publication status

published

Editor

Book title

Volume

5 (4)

Pages / Article No.

781 - 789

Publisher

Copernicus

Event

Edition / version

Methods

Software

Geographic location

Date collected

Date created

Subject

Organisational unit

08619 - Labor für Ionenstrahlphysik (LIP) / Laboratory of Ion Beam Physics (LIP) check_circle
03868 - Eglinton, Timothy I. (emeritus) / Eglinton, Timothy I. (emeritus) check_circle

Notes

Funding

140850 - Climate and Anthropogenic PerturbationS of Land-Ocean Carbon tracKs (CAPS-LOCK) (SNF)
163162 - Climate and Anthropogenic PerturbationS of Land-Ocean Carbon tracKs (CAPS-LOCK2) (SNF)

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