HR: 14:40h
AN: B53B-05 [Abstracts]
TI: Quantification of Calcium Isotope Fractionation in Ectomycorrhizal Trees
AU: * Hoff, C J
EM: choff@cisunix.unh.edu
AF: UNH Dept. of Earth Sciences, James Hall, Durham, NH 03824
United States
AU: Bryce, J G
EM: julie.bryce@unh.edu
AF: UNH Dept. of Earth Sciences, James Hall, Durham, NH 03824
United States
AU: Hobbie, E A
EM: erik.hobbie@unh.edu
AF: UNH Complex Systems Research Center, Morse Hall, Durham, NH 03824
United States
AU: Colpaert, J V
EM: jan.colpaert@luc.ac.be
AF: Limburgs Universitair Centrum, Environmental Biology Universitaire Campus, Diepenbeek, B-3590
Belgium
AU: Bullen, T D
EM: tdbullen@usgs.gov
AF: USGS Branch of Regional Research, Water Resources Division, MS 420, 345 Middlefield Rd., Menlo Park, CA
94025
United States
AB:
Calcium plays a significant role in many forest ecosystem processes and is required for plant growth. Within plants, calcium
is a critical component of cell walls and membranes, signaling processes, and charge balances (1). Current efforts to
quantify Ca cycling in ecosystems rely on large-scale ecosystem manipulations (e.g., 2) or mass balances (e.g., 3) and
indirect chemical proxies, Ca/Sr or Sr isotopic systems (e.g., 4). The measurement of Ca isotopes may provide more direct
information about the calcium sources and fluxes within and between the geological (mineral and soil) and biological (fungi
and plants) components of terrestrial ecosystems. To examine calcium isotopic variability systematically, we measured the
fractionation between roots and needles in cultured Scots pine ( Pinus sylvestris) seedlings. Our samples include roots
and needles from trees grown at low or high nutrient supply rates (3% or 5% per day). Because mycorrhizal fungi are
intimately involved in plant nutrient supply, we also tested whether mycorrhizal colonization by Suillus bovinus
affected calcium isotopic fractionation. Initial results demonstrate that at a low nutrient supply rate there is a small but
measurable fractionation (averaging 0.58 ‰) between the roots and needles of individual trees; the needles are
enriched in 40Ca compared to the roots. The root-needle fractionation is unaffected by mycorrhizal colonization. Ongoing
analyses will address both the consistency of the root-needle fractionation and the impacts of nutrient supply rate on
fractionation. Preliminary results suggest that higher nutrient supply rates lead to decreased root-needle fractionation.
Analyses underway will also address whether different fungal species ( Thelephora terrestris) affect the documented
root-needle fractionation. Isotope signatures of calcium source materials will complete our sample suite and will be used to
assess fractionation during uptake. Ultimately, the results of this study will provide important insights into models of
calcium isotope fractionation mechanisms as well as calcium cycling in forest ecosystems.
(1) White, P.J. and M.R. Broadley. 2003. Annals of Botany. 92:487-511.
(2) Peters, S.C., et al. 2004. Biogeochem. 67: 309-329.
(3) Schmitt, et al. 2003. EPSL. 6731: 1-16.
(4) Blum, J.D., et al. 2002. Nature. 417: 729-731.
DE: 0400 BIOGEOSCIENCES
DE: 0414 Biogeochemical cycles, processes, and modeling (0412, 0793, 1615, 4805, 4912)
DE: 0454 Isotopic composition and chemistry (1041, 4870)
DE: 0470 Nutrients and nutrient cycling (4845, 4850)
SC: Biogeosciences [B]
MN: Fall Meeting 2005