The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.
Where temperate meets tropical: multi‐factorial effects of elevated CO2, nitrogen enrichment, and competition on a mangrove‐salt marsh community
Abstract
Our understanding of how elevated CO 2 and interactions with other factors will affect coastal plant communities is limited. Such information is particularly needed for transitional communities where major vegetation types converge. Tropical mangroves (Avicennia germinans) intergrade with temperate salt marshes (Spartina alterniflora) in the northern Gulf of Mexico, and this transitional community represents an important experimental system to test hypotheses about global change impacts on critical ecosystems. We examined the responses of A. germinans (C 3) and S. alterniflora (C 4), grown in monoculture and mixture in mesocosms for 18 months, to interactive effects of atmospheric CO 2 and pore water nitrogen (N) concentrations typical of these marshes. A. germinans, grown without competition from S. alterniflora, increased final biomass (35%) under elevated CO 2 treatment and higher N availability. Growth of A. germinans was severely curtailed, however, when grown in mixture with S. alterniflora, and enrichment with CO 2 and N could not reverse this growth suppression. A field experiment using mangrove seedlings produced by CO 2‐ and N‐enriched trees confirmed that competition from S. alterniflora suppressed growth under natural conditions and further showed that herbivory greatly reduced survival of all seedlings. Thus, mangroves will not supplant marsh vegetation due to elevated CO 2 alone, but instead will require changes in climate, environmental stress, or disturbance to alter the competitive balance between these species. However, where competition and herbivory are low, elevated CO 2 may accelerate mangrove transition from the seedling to sapling stage and also increase above‐ and belowground production of existing mangrove stands, particularly in combination with higher soil N.
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Cites
Drought, Snails, and Large-Scale Die-Off of Southern U.S. Salt Marshes
Silliman, B. R., van de Koppel, J., Bertness, M. D., Stanton, L. E., & Mendelssohn, I. A. (2005) · Science · doi:10.1126/science.1118229 · Cited by 426
Cited by
Impacts of climate change on mangrove ecosystems: a region by region overview
Ward, R. D., Friess, D. A., Day, R. H., & Mackenzie, R. A. (2016) · Ecosystem Health and Sustainability · doi:10.1002/ehs2.1211 · Cited by 668
Organic carbon burial rates in mangrove sediments: strengthening the global budget
Breithaupt, J. L., Smoak, J. M., Smith, T. J., Sanders, C. J., & Hoare, A. (2012) · Global Biogeochemical Cycles · doi:10.1029/2012gb004375 · Cited by 428
Conservation and restoration of mangroves: Global status, perspectives, and prognosis
Romañach, S. S., DeAngelis, D. L., Koh, H. L., Li, Y., Teh, S. Y., Raja Barizan, R. S., & Zhai, L. (2018) · Ocean & Coastal Management · doi:10.1016/j.ocecoaman.2018.01.009 · Cited by 426
Mesocosm Experiments as a Tool for Ecological Climate-Change Research
Stewart, R. I. A., Dossena, M., Bohan, D. A., Jeppesen, E., Kordas, R. L., Ledger, M. E., Meerhoff, M., Moss, B., Mulder, C., Shurin, J. B., et al. (2013) · Advances in Ecological Research · doi:10.1016/b978-0-12-417199-2.00002-1 · Cited by 387
Metadata
- Authors
- McKEE, K. L., & ROOTH, J. E.
- Venue
- Global Change Biology
- Publisher
- Wiley
- Published
- 2008-01-20
- Volume
- 14
- Issue
- 5
- Pages
- 971-984
- ISSN
- 1354-1013 (ISSN-L)
- 1365-2486
- OpenAlex
- W2167976739
- Cited by
- 159
- References
- 1
- FWCI
- 3.11
- Type
- journal article
- Language
- en
- Open access
- closed
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- McKEE, K. L., & ROOTH, J. E. (2008). Where temperate meets tropical: multi‐factorial effects of elevated CO2, nitrogen enrichment, and competition on a mangrove‐salt marsh community. Global Change Biology. https://doi.org/10.1111/j.1365-2486.2008.01547.x
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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