4 Earth Biogeochemistry

Thursday, 31 March 2016
8:00 AM - 12:00 PM
Richland B


C:N:P RELATIONSHIPS ACROSS TIDAL AND SEASONAL TIME-SCALES WITHIN A SALT-MARSH ESTUARY

Paper number: 4-5
Program: Theme Sessions
Time: 9:20 AM – 9:40 AM


Authors

  • Doug Bell Presenting Author
    University of South Carolina, Columbia, SC

Abstract

Marsh-estuarine systems serve as an essential biogeochemical link between freshwater/terrestrial ecosystems and the marine biosphere. Within an estuary system, the relative inventories of carbon (C), nitrogen (N), and phosphorus (P) are significantly influenced through a variety of biotic and chemical transformations. While open ocean patterns of C, N, and P are relatively well studied, fewer efforts have been directed towards the dynamic estuary environment, despite the use of elemental stoichiometry in monitoring water quality and ecosystem function. Samples were collected over complete tidal cycles (24-hr diurnal period every 2 hrs) over the course of a seasonal cycle (effort conducted twice per environmental season) for inorganic and organic C, N, and P concentrations in particulate and dissolved material. This study was conducted within North Inlet, SC (NI), a well-studied site within the National Estuarine Research Reserve System (NERRS). NI is considered to be in relatively pristine ecosystem condition, providing assessment without complicating anthropogenic influences. NI also experiences significant turnover over a tidal cycle (55% volume; 3,300 hectares), which allowed for sampling at a single monitoring station to observe the transition of distinct signals from the salt marsh and the coastal ocean. To investigate potential mechanisms which shape observed C:N:P variability, bulk signatures of particulate 13C and isolated (via electrodialysis/reverse osmosis) dissolved organic material 13C and 15N are compared.

Geological Society of America Abstracts with Programs. Vol. 48, No. 3

doi: 10.1130/abs/2016SE-271891

© Copyright 2016 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.