Journal
ORGANIC GEOCHEMISTRY
Volume 41, Issue 3, Pages 281-290Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.orggeochem.2009.10.009
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Funding
- University of Otago [2006, 2007]
- William-Evans Fellowship
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The branched/isoprenoid tetraether (BIT) index has recently been proposed as a qualitative proxy for the relative amounts of soil and marine derived organic matter (OM) in marine sediments. We compare BIT values with lignin-phenol CuO oxidation products and bulk OM proxies in surface sediment samples from Doubtful Sound, a ford in the southwestern end of New Zealand's South Island, as well as in soils and leaf litter from the local pristine temperate rainforest watershed. The region has extreme rates of annual rainfall (>7 m year(-1)) and large mass-wasting soil and vegetation events on fjord slopes, which results in relatively high fluxes of terrestrial organic matter (OMterr) to fjord sediments. Sediments contained up to 11.4% w/w organic carbon (OC) with terrestrial to a mixture of terrestrial/marine delta C-13 (-24.3 parts per thousand to -28.7 parts per thousand) and C/N (14.7-36.8) signatures. BIT values ranged from 0.24 to 0.93. Lignin abundance in sediments, reported as Lambda(8) values (mg 8 lignin-phenols/100 mg OC-1), ranged from 2.7 to 11.2. A weak correlation was found between concentrations of lignin phenols and BIT values (R-2 0.313). The likely cause of the differences between the two proxies is differences in the relative amounts of soil OM (OMsoil) and vegetation (intact and detrital) transported to the fiord by episodic mass-wasting events and gradual accumulation from overland (leaching by rainfall) and riverine sources. Interestingly, the BIT index correlated significantly with bulk sedimentary OM (OMsed) proxies (delta C-13, R-2 0.774) (C/N, R-2 0.629), while lignin phenol values (Lambda(8)) exhibited a much weaker correlation with delta C-13 values (R-2 0.320) and no correlation with C/N values (R-2 0.005). This suggests that OMsoil represents the dominant fraction of OMterr delivered to fjord sediments. (C) 2009 Elsevier Ltd. All rights reserved.
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