Tracing Mississippi River influences in estuarine food webs of coastal Louisiana

被引:76
|
作者
Wissel, B
Fry, B
机构
[1] Univ Regina, Fac Sci, Regina, SK S4S 0A2, Canada
[2] Louisiana State Univ, Dept Oceanog & Coastal Studies, Coastal Ecol Inst, Baton Rouge, LA 70803 USA
基金
美国海洋和大气管理局;
关键词
carbon; nitrogen and sulfur stable isotopes; mixing models; estuaries; Mississippi River; primary consumers;
D O I
10.1007/s00442-005-0119-z
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The Breton Sound estuary in southern Louisiana receives large amounts of Mississippi River water via a controlled diversion structure at the upstream end of the estuary. We used stable isotopes to trace spatial and seasonal responses of the downstream food web to winter and spring introductions of river water. Analysis of delta(13)C, delta(15)N, and delta(34)S in the common local consumers such as grass shrimp (Palaemonetes sp.), barnacles (Balanus sp.), and small plankton-feeding fish (bay anchovies, Anchoa mitchilli) showed that the diversion was associated with two of the five major source regimes that were supporting food webs: a river regime near the diversion and a river-influenced productive marsh regime farther away from the diversion. Mixing models identified a third river-influenced source regime at the marine end of the estuary where major natural discharge from the Bird's Foot Delta wraps around into estuarine waters. The remaining two source regimes represented typical estuarine conditions: local freshwater sources especially from precipitation and a brackish source regime representing higher salinity marine influences. Overall. the Mississippi River diversion accounted for 75% of food web support in the upper estuary and 25% in the middle estuary, with influence strongest along known flow pathways and closest to the diversion. Isotopes also traced seasonal changes in river contributions, and indicated increased plant community productivity along the major flow path of diversion water. In the Breton Sound estuary, bottom-up forcing of food webs is strongly linked to river introductions and discharge, occurring in spatial and temporal patterns predictable from known river input regimes and known hydrologic circulation patterns.
引用
收藏
页码:659 / 672
页数:14
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