Latitudinal trends in Spartina alterniflora productivity and the response of coastal marshes to global change

被引:191
作者
Kirwan, Matthew L. [1 ]
Guntenspergen, Glenn R. [2 ]
Morris, James T. [3 ]
机构
[1] Univ Virginia, Dept Environm Sci, Patuxent Wildlife Res Ctr, US Geol Survey, Charlottesville, VA 22904 USA
[2] US Geol Survey, Patuxent Wildlife Res Ctr, Laurel, MD USA
[3] Univ S Carolina, Belle W Baruch Inst Marine Biol & Coastal Res, Columbia, SC 29208 USA
基金
美国国家科学基金会;
关键词
biomass; climate; sea level; temperature; warming; wetland; SEA-LEVEL RISE; GENETIC DIVERSITY; TIDAL MARSH; CO2; GROWTH; BAY; CORDGRASS; DYNAMICS; PATTERNS; IMPACTS;
D O I
10.1111/j.1365-2486.2008.01834.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Marshes worldwide are actively degrading in response to increased sea level rise rates and reduced sediment delivery, though the growth rate of vegetation plays a critical role in determining their stability. We have compiled 56 measurements of aboveground annual productivity for Spartina alterniflora, the dominant macrophyte in North American coastal wetlands. Our compilation indicates a significant latitudinal gradient in productivity, which we interpret to be determined primarily by temperature and/or the length of growing season. Simple linear regression yields a 27 g m(-2) yr(-1) increase in productivity with an increase of mean annual temperature by 1 degrees C. If temperatures warm 2-4 degrees C over the next century, then marsh productivity may increase by 10-40%, though physiological research suggests that increases in the north could potentially be offset by some decreases in the south. This increase in productivity is roughly equivalent to estimates of marsh lost due to future sea level change. If a warming-induced stimulation of vegetation growth will enhance vertical accretion and limit erosion, then the combined effects of global change may be to increase the total productivity and ecosystem services of tidal wetlands, at least in northern latitudes.
引用
收藏
页码:1982 / 1989
页数:8
相关论文
共 51 条
[41]   River forcing at work: Ecological modeling of prograding and regressive deltas [J].
Reyes E. ;
Martin J.F. ;
Day J.W. ;
Kemp G.P. ;
Mashriqui H. .
Wetlands Ecology and Management, 2004, 12 (2) :103-114
[42]   RESPONSE TO PHOTOPERIOD AND TEMPERATURE BY SPARTINA-ALTERNIFLORA (POACEAE) FROM NORTH-CAROLINA AND SPARTINA-FOLIOSA FROM CALIFORNIA [J].
SENECA, ED ;
BLUM, U .
AMERICAN JOURNAL OF BOTANY, 1984, 71 (01) :91-99
[43]  
Shea M.L., 1977, Photosynthesis and Photorespiration in Relation to the Phenotypic Forms of Spartina Alterniflora
[44]  
Smalley A.E., 1958, Doctoral Dissertaion
[45]   Interannual variability of a salt-marsh ecosystem [J].
Teal, JM ;
Howes, BL .
LIMNOLOGY AND OCEANOGRAPHY, 1996, 41 (04) :802-809
[46]   Vegetation causes channel erosion in a tidal landscape [J].
Temmerman, S. ;
Bouma, T. J. ;
Van de Koppel, J. ;
Van der Wal, D. ;
De Vries, M. B. ;
Herman, P. M. J. .
GEOLOGY, 2007, 35 (07) :631-634
[47]  
TITUS JG, 1988, 2300586013 US EPA
[48]   A comparative assessment of genetic diversity among differently-aged populations of Spartina alterniflora on restored versus natural wetlands [J].
Travis, SE ;
Proffitt, CE ;
Lowenfeld, RC ;
Mitchell, TW .
RESTORATION ECOLOGY, 2002, 10 (01) :37-42
[49]  
TURNER RE, 1976, CONTRIB MAR SCI, V20, P47
[50]   Patterns, rates and possible causes of saltmarsh erosion in the Greater Thames area (UK) [J].
van der Wal, D ;
Pye, K .
GEOMORPHOLOGY, 2004, 61 (3-4) :373-391