Responses of Spartina alterniflora to Multiple Stressors: Changing Precipitation Patterns, Accelerated Sea Level Rise, and Nutrient Enrichment

被引:0
作者
Alana Hanson
Roxanne Johnson
Cathleen Wigand
Autumn Oczkowski
Earl Davey
Erin Markham
机构
[1] U.S. Environmental Protection Agency,Atlantic Ecology Division
[2] University of Rhode Island,Graduate School of Oceanography
来源
Estuaries and Coasts | 2016年 / 39卷
关键词
Salt marsh; Climate change; Precipitation; Sea level rise; Eutrophication;
D O I
暂无
中图分类号
学科分类号
摘要
Coastal wetlands, well recognized for their ecosystem services, have faced many threats throughout the USA and elsewhere. While managers require good information on the net impact of these combined stressors on wetlands, little such information exists. We conducted a 4-month mesocosm study to analyze the multiple stressor effects of precipitation changes, sea level rise, and eutrophication on the salt marsh plant Spartina alterniflora. Pots containing plants in an organic soil matrix were positioned in tanks and received Narragansett Bay (RI, USA) water. The study simulated three precipitation levels (ambient daily rain, biweekly storm, and drought), three levels of tidal inundations (high (15 cm below mean high water (MHW)), mean (MHW), and low (15 cm above MHW)), and two nutrient enrichment levels (unenriched and nutrient-enriched bay water). Our results demonstrate that storm and drought stressors led to significantly less above- and belowground biomass than those in ambient rain conditions. Plants that were flooded at high inundation had less belowground biomass, fine roots, and shoots. Nutrients had no detectable effect on aboveground biomass, but the enriched pots had higher stem counts and more fine roots than unenriched pots, in addition to greater CO2 emission rates; however, the unenriched pots had significantly more coarse roots and rhizomes, which help to build peat in organogenic marshes. These results suggest that multiple stressors of altered precipitation, sea level rise, and nutrient enrichment would lead to reduced marsh sustainability.
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页码:1376 / 1385
页数:9
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共 152 条
  • [1] Allen JRL(1990)The formation of coastal peat marshes under an upward tendency of relative sea-level Journal of the Geological Society of London 147 743-745
  • [2] Beier C(2012)Precipitation manipulation experiments—challenges and recommendations for the future Ecology Letters 15 899-911
  • [3] Beierkuhnlein C(2012)Evidence of sea level acceleration at U.S. and Canadian tide stations, Atlantic coast, North America Journal of Coastal Research 28 1437-1445
  • [4] Wohlgemuth T(2010)Climate change, sea-level rise, and coastal wetlands National Wetlands Newsletter 32 8-12
  • [5] Peñuelas J(2009)Effects of warming and altered precipitation on plant and nutrient dynamics of a New England salt marsh Ecological Applications 19 1758-1773
  • [6] Emmett B(2011)Sea-level rise from the late 19th to the early 21st century Surveys in Geophysics 32 585-602
  • [7] Körner C(2008)Interactive and cumulative effects of multiple human stressors in marine systems Ecology Letters 11 1304-1315
  • [8] de Boeck H(2011)Use of computed tomography imaging for quantifying coarse roots, rhizomes, peat, and particle densities in marsh soils Ecological Applications 21 2156-2171
  • [9] Hesselbjerg Christensen J(2012)Coastal eutrophication as a driver of marsh loss Nature 490 388-392
  • [10] Leuzinger S(2012)Numerical models of salt marsh evolution: ecological, geomorphic, and climatic factors Reviews of Geophysics 50 445-458