Macrofaunal recolonization on intertidal mudflats: effect of sediment organic and sand content

被引:49
作者
Bolam, SG
Whomersley, P
Schratzberger, M
机构
[1] Ctr Environm Fisheries & Aquaculture Sci, Burnham Lab, Burnham On Crouch CM0 8HA, Essex, England
[2] Ctr Environm Fisheries & Aquaculture dSci, Lowestoft Lab, Lowestoft NR33 0HT, Suffolk, England
关键词
mudflat; organic content; particle size; recolonization; scale;
D O I
10.1016/j.jembe.2004.01.007
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Following concerns over how differences in dredged material properties affects recovery following dredged material deposition on mudflats, a field manipulation experiment was conducted to investigate the effects of increased sediment organic content (from 0.9% to 2.8%) and sand content (from 12.0% to 47.0%) on macrofaunal recolonization and sediment properties on an intertidal mudflat, Crouch Estuary, Essex, UK. The manipulated sediments were placed in 1-m(2) plots, 10 cm, deep, in a randomised block design and macrofauna and sediments sampled after 1 week, 1, 3, 6, and 12 months. The results suggested that while increased sand content had no discernible effect on sediment property changes, increased organic content resulted in marked reductions in redox potential at 1-, 2- and 4-cm sediment depths and increased shear strengths. These sediments exhibited a distinct 'cracking' appearance on their surfaces. Similarly, while macrofaunal recovery was only affected by increased sand content in the short-term (1 month), total numbers of individuals, number of species and diversity took longer to recover in sediments with increased organic contents. Recolonization proceeded via a gradual increase in the abundance of those taxa present in ambient sediments rather than via a distinct successional sequence. Recovery was species-specific with two species (Hediste diversicolor (Muller) and Hydrobia ulvae (Pennant)) recovering to ambient levels within the first week of the experiment. Multivariate analyses indicated that the community assemblages of the low-organic content treatments had recovered after 12 months while those of the high-organic content treatments were still significantly different to those of the controls at the end of the experiment. We propose that the relatively rapid recovery and lack of successional sequence generally observed in all sediment types of this study can be explained by the opportunistic nature of the ambient assemblage and by the dispersive nature of the dominant species. Reduced sediments and/or increased shear strengths led to a slow recovery in high-organic content treatments. These results indicate that a careful consideration of the organic content of fine-grained dredged material must be made during the licensing process of beneficial use schemes. Crown Copyright (C) 2004 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:157 / 180
页数:24
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