MEPS 252:51-60 (2003)  -  doi:10.3354/meps252051

Nitrogen and carbon isotopic composition of high-molecular-weight dissolved organic matter in marine environments

Laodong Guo1,*, Noriyuki Tanaka1, Donald M. Schell2, Peter H. Santschi3

1International Arctic Research Center, and
2Institute of Marine Science, University of Alaska Fairbanks, Alaska 99775, USA
3Department of Oceanography, Texas A&M University, Galveston, Texas 77551, USA

ABSTRACT: High-molecular-weight (HMW) dissolved organic matter (DOM) was isolated using cross-flow ultrafiltration from seawater across a salinity gradient in 2 estuarine/coastal marine environments‹Chesapeake Bay/Middle Atlantic Bight (MAB) and Galveston Bay/Gulf of Mexico. Nitrogen and carbon isotope ratios (δ15N and δ13C) were measured on the isolated HMW DOM samples (defined here as the size fraction between 1 and 200 nm), which made up ~50 to 60% of the total DOM in the estuarine regions and decreased to ~35% of the DOM at the MAB and Gulf of Mexico stations. δ15N values varied from 4.8 to 8.1” in the Chesapeake Bay/MAB area. In the Galveston Bay/Gulf of Mexico region, δ15N and δ13C values varied from 3.2 to 9.5” and -26.1 to -20.9”, respectively. Similar distribution patterns of δ13C and δ15N were observed in both study areas, with values of δ15N showing a mid-salinity maximum of about 8 to 10”, whereas δ13C continually increased with increasing salinity. The δ13C values clearly demonstrated a shift of HMW organic carbon sources from largely terrestrial inputs in the upper-estuarine areas to marine-dominated organic carbon sources in lower-estuarine and coastal regions. The more complicated distribution patterns of δ15N, with δ15N values first increasing with salinity in estuarine regions then decreasing towards the seawater endmember, suggest more dynamic N cycling. Thus, in addition to organic matter sources, biogeochemical and isotopic fractionation processes are important factors governing marine HMW DOM δ15N values. Vertical profiles of HMW DOM δ13C in open-ocean stations generally decrease from surface water to deep waters, whereas the opposite was found for δ15N. HMW DOM components with heavier δ13C and lighter δ15N values seem to be preferentially degraded during their transport from surface to deep waters. However, other processes could also have contributed to this distribution trend. While the carbon isotopic signature can be used as an indicator of DOM sources, nitrogen isotopic composition, on the other hand, appears to be related to both source functions and subsequent recycling in marine environments. Comparisons of δ15N with previously published Δ14C values for the same samples support these conclusions about possible 15N degradation pathways.


KEY WORDS: Dissolved organic matter · Stable isotopes · Colloids · Estuary · Ultrafiltration · Seawater


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