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Citation
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HERO ID
2653555
Reference Type
Journal Article
Title
Temporal buffering of climate-driven sediment flux cycles by transient catchment response
Author(s)
Armitage, JJ; Dunkley Jones, Tom; Duller, RA; Whittaker, AC; Allen, PA
Year
2013
Is Peer Reviewed?
Yes
Journal
Earth and Planetary Science Letters
ISSN:
0012-821X
EISSN:
1385-013X
Volume
369
Page Numbers
200-210
DOI
10.1016/j.epsl.2013.03.020
Web of Science Id
WOS:000320684500020
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 ( <10(6) yr) climatic cycles, and whether particulate sediment flux signals can be expected to be recorded in the clastic sedimentary record of adjacent basin-fills. Recent field and theoretical studies suggest that mountain catchments respond transiently to high frequency forcing, and so sediment discharge from the catchment is a non-linear function of forcing variables. Using a catchment basin model, we demonstrate that climate-driven cyclicity in particulate sediment discharge is strongly damped when the period of climate variability is shorter than the response timescale of the eroding landscape. Given that the response timescale of landscapes is of the order of 10(6) yr, and that Milankovitch-driven climate cyclicity is of the order of 10(4)-10(5) yr, it is likely that climate-driven perturbation of upland catchments at these periods will be strongly damped by transient landscape behaviour. Our results therefore suggest that stratigraphy built by particulate fluxes from upland catchments, and long-term trends in the sediment delivery to the ocean, may be relatively insensitive to short-term climate variability. (C) 2013 Elsevier B.V. All rights reserved.
Keywords
stratigraphy; climate change; landscape evolution
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