Articles | Volume 5, issue 6
Biogeosciences, 5, 1693–1704, 2008
Biogeosciences, 5, 1693–1704, 2008

  11 Dec 2008

11 Dec 2008

Unusually negative nitrogen isotopic compositions (δ15N) of mangroves and lichens in an oligotrophic, microbially-influenced ecosystem

M. L. Fogel1, M. J. Wooller1,2, J. Cheeseman3, B. J. Smallwood4,5, Q. Roberts1,5, I. Romero5, and M. J. Meyers5 M. L. Fogel et al.
  • 1Carnegie Institution of Washington, Geophysical Laboratory, 5251 Broad Branch Rd., NW, Washington, DC 20015, USA
  • 2Alaska Stable Isotope Facility: Water and Environmental Research Center, Institute of Marine Science and School of Fisheries and Ocean Sciences, University of Alaska, Fairbanks, Alaska, 99775, USA
  • 3Department of Plant Biology, University of Illinois, Urbana, Illinois, 61801, USA
  • 4Department of Oceanography, Texas A&M, College Station, Texas, 77843-3146, USA
  • 5University of Southern California, 3616 Trousdale Parkway, Los Angeles, California, 90089, USA

Abstract. Extremes in δ15N values in mangrove tissues and lichens (range =+4 to −22‰) were measured from a mangrove forest ecosystem located on Twin Cays, offshore islands in Belize, Central America. The N isotopic compositions and concentrations of NH4+/NH3 in porewater, rainwater, and atmospheric ammonia, and the δ15N of lichens, mangrove leaves, roots, stems, and wood were examined to study the biogeochemical processes important for establishing these unusual N isotopic ratios. Dwarfed Rhizophora mangle trees had the most negative δ15N, whereas fringing Rhizophora trees, the most positive δ15N values. Porewater ammonium concentrations had little relationship to N isotopic fractionation in mangrove tissues. In dwarfed mangroves, the δ15N of fine and coarse roots were 6–9‰ more positive than leaf tissue from the same tree, indicating different sources of N for root and leaf tissues. When P was added to dwarfed mangrove trees without added N, δ15N increased within one year from −12‰ to −2‰, approaching the δ15N of porewater ammonium (δ15N=+4‰). Isotopically depleted ammonia in the atmosphere (δ15N=−19‰) and in rainwater (δ15N=−10‰) were found on Twin Cays. We propose that foliar uptake of these atmospheric sources by P-stressed, dwarfed mangrove trees and lichens can explain their very negative δ15N values. In environments where P is limiting for growth, uptake of atmospheric N by Rhizophora mangle may be an important adaptive strategy.

Final-revised paper