Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/11434
Title: Carbon isotope fractionation in the mangrove Avicennia marina has implications for food web and blue carbon research
Authors: Kelleway, JJ
Mazumder, D
Baldock, JA
Saintilan, N
Keywords: Carbon
Stable isotopes
Ecology
Ecosystems
Mangroves
Estuaries
Habitat
Issue Date: 31-May-2018
Publisher: Elsevier B. V.
Citation: Kelleway, J. J., Mazumder, D., Baldock, J. A., & Saintilan, N. (2018). Carbon isotope fractionation in the mangrove Avicennia marina has implications for food web and blue carbon research. Estuarine, Coastal and Shelf Science, 205, 68-74. doi:10.1016/j.ecss.2018.03.011
Abstract: The ratio of stable isotopes of carbon (δ13C) is commonly used to track the flow of energy among individuals and ecosystems, including in mangrove forests. Effective use of this technique requires understanding of the spatial variability in δ13C among primary producer(s) as well as quantification of the isotopic fractionations that occur as C moves within and among ecosystem components. In this experiment, we assessed δ13C variation in the cosmopolitan mangrove Avicennia marina across four sites of varying physico-chemical conditions across two estuaries. We also compared the isotopic values of five distinct tissue types (leaves, woody stems, cable roots, pneumatophores and fine roots) in individual plants. We found a significant site effect (F3, 36 = 15.78; P < 0.001) with mean leaf δ13C values 2.0‰ more depleted at the lowest salinity site compared to the other locations. There was a larger within-plant fractionation effect, however, with leaf samples (mean ± SE = −29.1 ± 0.2) more depleted in 13C than stem samples (−27.1 ± 0.1), while cable root (−25. 8 ± 0.1), pneumatophores (−25.7 ± 0.1) and fine roots (−26.0 ± 0.2) were more enriched in 13C relative to both aboveground tissue types (F4, 36 = 223.45; P < 0.001). The within-plant δ13C fractionation we report for A. marina is greater than that reported in most other ecosystems. This has implications for studies of estuarine carbon cycling. The consistent and large size of the fractionation from leaf to woody stem (∼2.0‰) and mostly consistent fractionation from leaf to root tissues (>3.0‰) means that it may now be possible to partition the individual contributions of various mangrove tissues to estuarine food webs. Similarly, the contributions of mangrove leaves, woody debris and belowground sources to blue carbon stocks might also be quantified. Above all, however, our results emphasize the importance of considering appropriate mangrove tissue types when using δ13C to trace carbon cycling in estuarine systems..© 2018 Elsevier Ltd
URI: https://doi.org/10.1016/j.ecss.2018.03.011
https://apo.ansto.gov.au/dspace/handle/10238/11434
ISSN: 0272-7714
Appears in Collections:Journal Articles

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.