SALT-MARSH DEVELOPMENT STUDIES AT WAQUOIT BAY, MASSACHUSETTS - INFLUENCE OF GEOMORPHOLOGY ON LONG-TERM PLANT COMMUNITY STRUCTURE

被引:44
作者
ORSON, RA
HOWES, BL
机构
[1] WOODS HOLE OCEANOG INST,DEPT BIOL,WOODS HOLE,MA 02543
[2] WILLIAM PATERSON STATE COLL,DEPT GEOG & ENVIRONM SCI,WAYNE,NJ 07470
关键词
PALEOECOLOGY; GEOMORPHOLOGY; PLANT COMMUNITY STRUCTURE; NEW-ENGLAND COAST;
D O I
10.1016/S0272-7714(05)80025-3
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
Stochastic events relating to beach formation and inlet dynamics have been the major factors influencing the development of the Waquoit Bay tidal marshes. This results from the physical structure of the Waquoit Bay system where tidal exchange is limited to one or two small inlets and is in contrast to marsh development in nearby Barnstable Marsh where direct unrestricted exchange with Cape Cod Bay has smoothed the effects of stochastic events on vegetation development. We contend that vegetation development in salt marshes where connections to adjacent waters are restricted will be dominated by abiotic factors (e.g. storms, sedimentation rates, etc.) while those marshes directly linked to open bodies of water and where alterations to hydrodynamic factors are gradual, autecological processes (e.g. interspecific competition) will dominate long-term plant community development. The results from the five marsh systems within the Waquoit Bay complex suggest that once a vegetation change occurs the new community tended to persist for long periods of time (100's-1000's years). Stability of the 'new' community appeared to depend upon the stability of the physical structure of the system and/or time between perturbations necessary to allow the slower autecological processes to have a discernable effect. In order for the plant community to persist as long as observed, the vegetation must also be exerting an influence on the processes of development. Increased production of roots and rhizomes and growth characteristics (density of culms) are some of the factors which help to maintain long-term species dominance. It is clear from this investigation that the structure of the plant community at any one point in time is dependent upon numerous factors including historical developmental influences. To properly assess changes to the present plant community or determine recent rates of accretion, historic developmental trends must be considered. The factors that have influenced the development of marsh in the past will be important in understanding and formulating predictive models in the future. © 1992 Academic Press Limited.
引用
收藏
页码:453 / 471
页数:19
相关论文
共 35 条
[1]   FACTORS INFLUENCING VASCULAR PLANT ZONATION IN NORTH-CAROLINA SALT MARSHES [J].
ADAMS, DA .
ECOLOGY, 1963, 44 (03) :445-+
[2]  
[Anonymous], 1967, GEOGR ANN
[3]   SUBMERGENCE OF CONNECTICUT COAST [J].
BLOOM, AL ;
STUIVER, M .
SCIENCE, 1963, 139 (355) :332-&
[4]  
CHAPMAN VJ, 1960, SALT MARSHES SALT DE, P382
[5]   SPARTINA IN MARIAGER FJORD, DENMARK - THE EFFECT ON SEDIMENT PARAMETERS [J].
CHRISTIANSEN, C ;
MILLER, PF .
EARTH SURFACE PROCESSES AND LANDFORMS, 1983, 8 (01) :55-62
[6]   THE DEVELOPMENT OF A TIDAL MARSH - UPLAND AND OCEANIC INFLUENCES [J].
CLARK, JS ;
PATTERSON, WA .
ECOLOGICAL MONOGRAPHS, 1985, 55 (02) :189-&
[7]  
Davis C.A., 1910, ECON GEOL, V5, P623, DOI DOI 10.2113/GSECONGEO.5.7.623
[8]  
Emery K. O., 1991, SEA LEVELS LAND LEVE
[9]  
Faure G., 1986, PRINCIPLES ISOTOPE G, V2nd, P347
[10]  
FLESSA K W, 1977, Chesapeake Science, V18, P172, DOI 10.2307/1350858