Historical Changes in the Vegetated Area of Salt Marshes

被引:28
作者
Burns, Christine J. [1 ,2 ]
Alber, Merryl [1 ]
Alexander, Clark R. [1 ,2 ]
机构
[1] Univ Georgia, Dept Marine Sci, Athens, GA 30602 USA
[2] Univ Georgia, Skidaway Inst Oceanog, Savannah, GA 31411 USA
关键词
Salt marsh; LTER; Image analysis; Ponding; Marsh migration; SEA-LEVEL RISE; EROSION; RESILIENCE; MIGRATION; COLLAPSE; UPLAND; BAY;
D O I
10.1007/s12237-020-00781-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Salt marshes are valuable ecosystems, and there is concern that increases in the rate of sea level rise along with anthropogenic activities are leading to the loss of vegetated habitat. The area of vegetated marsh can change not only through advance and retreat of the open fetch edge, but also due to channel widening and contracting, formation and drainage of interior ponds, formation and revegetation of interior mud flats, and marsh migration onto upland areas, each of which is influenced by different processes. This study used historical aerial photographs to measure changes in the extent of vegetated marsh over approximately 70 years at study marshes located in three long-term ecological research (LTER) sites along the US East coast: Georgia Coastal Ecosystems (GCE), Virginia Coast Reserve (VCR), and Plum Island Ecosystems (PIE). Marsh features were categorized into vegetated marsh, ponds, interior mud flats, and channels for three time periods at each site. The three sites showed different patterns of change in vegetated marsh extent over time. At the GCE study site, losses in vegetated marsh, which were primarily due to channel widening, were largely offset by channel contraction in other areas, such that there was little to no net change over the study period. The study marsh at VCR experienced extensive vegetated marsh loss to interior mud flat expansion, which occurred largely in low-lying areas. However, this loss was counterbalanced by marsh gain due to migration onto the upland, resulting in a net increase in vegetated marsh area over time. Vegetated marsh at PIE decreased over time due to losses from ponding, channel widening, and erosion at the open fetch marsh edge. Digital elevation models revealed that the vegetated areas of the three marshes were positioned at differing elevations relative to the tidal frame, with PIE at the highest and VCR at the lowest elevation. Understanding the patterns of vegetation loss and gain at a given site provides insight into what factors are important in controlling marsh dynamics and serves as a guide to potential management actions for marsh protection.
引用
收藏
页码:162 / 177
页数:16
相关论文
共 60 条
[1]   New England salt marsh pools: A quantitative analysis of geomorphic and geographic features [J].
Adamowicz, SC ;
Roman, CT .
WETLANDS, 2005, 25 (02) :279-288
[2]   Salt Marsh Dieback: An overview of recent events in the US [J].
Alber, Merryl ;
Swenson, Erick M. ;
Adamowicz, Susan C. ;
Mendelssohn, Irving A. .
ESTUARINE COASTAL AND SHELF SCIENCE, 2008, 80 (01) :1-11
[3]   The value of estuarine and coastal ecosystem services [J].
Barbier, Edward B. ;
Hacker, Sally D. ;
Kennedy, Chris ;
Koch, Evamaria W. ;
Stier, Adrian C. ;
Silliman, Brian R. .
ECOLOGICAL MONOGRAPHS, 2011, 81 (02) :169-193
[4]   Long-Term Erosional Trends Along Channelized Salt Marsh Edges [J].
Browne, James P. .
ESTUARIES AND COASTS, 2017, 40 (06) :1566-1575
[5]   Sea-Level Rise from the Late 19th to the Early 21st Century [J].
Church, John A. ;
White, Neil J. .
SURVEYS IN GEOPHYSICS, 2011, 32 (4-5) :585-602
[6]   Latent impacts: the role of historical human activity in coastal habitat loss [J].
Coverdale, Tyler C. ;
Herrmann, Nicholas C. ;
Altieri, Andrew H. ;
Bertness, Mark D. .
FRONTIERS IN ECOLOGY AND THE ENVIRONMENT, 2013, 11 (02) :69-74
[7]   Multiple stressors and the potential for synergistic loss of New England salt marshes [J].
Crotty, Sinead M. ;
Angelini, Christine ;
Bertness, Mark D. .
PLOS ONE, 2017, 12 (08)
[8]   On the tidal prism - channel area relations [J].
D'Alpaos, Andrea ;
Lanzoni, Stefano ;
Marani, Marco ;
Rinaldo, Andrea .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2010, 115
[9]  
Day JW, 1998, J COASTAL RES, V14, P583
[10]  
Dewberry, 2015, E SHORE VIRGINIA QL2