Temporal buffering of climate-driven sediment flux cycles by transient catchment response

J.J. Armitage; T. Dunkley Jones; R.A. Duller; A.C. Whittaker; P.A. Allen

doi:10.1016/j.epsl.2013.03.020

Temporal buffering of climate-driven sediment flux cycles by transient catchment response

J.J. Armitage
, T. Dunkley Jones
, R.A. Duller
, A.C. Whittaker
, P.A. Allen

Earth and Environmental Sciences

Research output: Contribution to journal › Article › peer-review

58 Citations (Scopus)

Abstract

The marine sedimentary record can exhibit a systematic cyclicity that is consistent with climate variability driven by Milankovitch-scale forcing. Milankovitch-band cyclicity is widely interpreted in the hemipelagic and pelagic sediments of the marine realm, and in terrestrial paleoenvironments has been observed in lacustrine sediments, soils and river floodplain successions. It remains unclear, however, if and how mountain catchments, as a primary sediment source, respond to these high frequency (

Original language	English
Pages (from-to)	200-210
Number of pages	11
Journal	Earth and Planetary Science Letters
Volume	369-370
DOIs	https://doi.org/10.1016/j.epsl.2013.03.020
Publication status	Published - 1 May 2013

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

SDG 14 Life Below Water
SDG 15 Life on Land

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10.1016/j.epsl.2013.03.020

Cite this

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AU - Allen, P.A.

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Temporal buffering of climate-driven sediment flux cycles by transient catchment response

Abstract

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