摘要

Reconstructing terrestrial water budgets is of prime importance for understanding past climate and environment. To shed more light on how plant-wax derived n-alkanes may be used for this purpose we investigated the distribution and stable isotopic compositions of hydrogen (delta D) and carbon (delta C-13) of plant-wax derived n-C-29 and -C-31 alkanes in terrestrial, coastal and offshore surface sediments in relation to hydrology along a NW-SE transect east of the Italian Apennines from the Po River to the Eastern Gulf of Taranto. The plant wax average chain length increases southward and may relate to increasing temperature and/or aridity. The plant wax delta D of the terrestrial and coastal samples also increases southward and mainly reflects changes in the delta D of precipitation. The delta C-13 of plant waxes is primarily interpreted in terms of C-3 vegetation changes rather than varying contributions by C-4 plants. The plant wax delta C-13-delta D composition of the Po River and Apennine rivers differs considerably from that in southern Italy, and suggests a mainly southern source for plant waxes in marine sediments of the Gulf of Taranto. This calibration provides a basis for the reconstruction of past changes in the Italian water balance and n-alkane source areas.

  • 出版日期2013-9-15

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