TY - JOUR
T1 - Temporal buffering of climate-driven sediment flux cycles by transient catchment response
AU - Armitage, J.J.
AU - Dunkley Jones, T.
AU - Duller, R.A.
AU - Whittaker, A.C.
AU - Allen, P.A.
PY - 2013/5/1
Y1 - 2013/5/1
N2 - 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 (
AB - 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 (
UR - http://www.scopus.com/inward/record.url?eid=2-s2.0-84878178265&partnerID=8YFLogxK
U2 - 10.1016/j.epsl.2013.03.020
DO - 10.1016/j.epsl.2013.03.020
M3 - Article
AN - SCOPUS:84878178265
SN - 0012-821X
VL - 369-370
SP - 200
EP - 210
JO - Earth and Planetary Science Letters
JF - Earth and Planetary Science Letters
ER -
