Distribution of terrigenous lipids in marine sediments off northeastern Taiwan
Resource
Deep Sea Research Part II: Topical Studies in Oceanography 50 (6-7): 1179-1201
Journal
Deep-Sea Research Part II: Topical Studies in Oceanography
Journal Volume
50
Journal Issue
6-7
Pages
1179-1201
Date Issued
2003
Author(s)
Abstract
Surface sediments on the continental margin off northeastern Taiwan have been analyzed for terrigenous lipids including n-alkanes, n-fatty alcohols, and sterols. Marine input to the sediments is particularly low based on the average n-C17/n-C29 alkane and n-C16/n-C28 fatty alcohol ratios, 0.15±0.13 and 0.13±0.06, respectively; this may be due to the fact that marine lipids are more prone to degradation than terrestrial ones. The study area has the highest plant wax n-alkane contribution (average carbon preference index 3.9±1.2) among the coastal marine areas surrounding Taiwan; lateral particle transport from the southern East China Sea shelf and river runoff from the east Taiwan coast are considered to be the major contributors. The distributions of plant wax n-alkane and n-alkanol concentrations normalized to total organic carbon (TOC) in the study area generally show maximum values on the upper slope of the southernmost Okinawa Trough, but not for phytosterols. Linear regression of TOC versus plant wax n-alkane concentrations show a weak relationship (r = 0.64, p = 0.001), and an even weaker relationship (r = 0.42, p = 0.05) between TOC and plant wax n-fatty alcohol concentrations is found. This could be attributed to several factors: (1) a complex input (not a point source) of terrigenous organic matter to the study area, (2) TOC also including marine organic matter, (3) temporal variations in river flow due to flooding, and (4) different rates of degradation for TOC and individual biomarkers. However, in spite of those factors, TOC and phytosterol concentrations are positively linearly correlated (r = 0.85, p<0.001), implying that the dilution of phytosterols in terrigenous organic carbon with marine organic carbon with or without the phytosterols follows a nearly constant ratio, which is remarkable. In addition, the predominant source of diploptene in the sediments does not appear to be of higher plant origin. © 2003 Elsevier Science Ltd. All rights reserved.
SDGs
Other Subjects
Alcohols; Coastal zones; Flow of fluids; Lipids; Sediments; Marine sediments; Marine biology; continental margin; lipid; marine sediment; terrigenous deposit; total organic carbon; (South); East China Sea; Embryophyta
Type
journal article
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