Macrofaunal responses to pit–mound patch dynamics in an intertidal mudflat: local versus patch-type effects

• Published in: Journal of experimental marine biology and ecology 2004-12, Vol.313 (2), p.297-315
• Main Author: Zajac, Roman N.
• Format: Article
• Language: English
• Subjects: Animal and plant ecology; Animal, plant and microbial ecology; Biological and medical sciences; Brackish; Colonization; Disturbance; Fundamental and applied biological sciences. Psychology; Macrofauna; Mounds; Mudflat; Patch Dynamics; Pits; Sea water ecosystems; Synecology
• ISSN: 0022-0981; 1879-1697
• DOI: 10.1016/j.jembe.2004.08.011

Biogenic structures created via feeding activities have varying effects on soft sediment communities, altering population dynamics, creating a temporal mosaic of successional patches, and ultimately increasing variation at different spatial scales. This study focused on assessing population responses to pits (P) and mounds (M) in an intertidal mudflat (River Plym, England) in order to determine (a) how these structures (max size 1400 cm 2), and their formation, affected infauna and (b) to what extent local variations in ambient communities may have affected infaunal responses. Densities in 0- and 1-week-old pits were significantly lower than in ambient and mound areas for most of the dominant infauna over the study period. Abundances were higher in mounds for some species and responses to both structures differed among juveniles and adults. Recovery to ambient levels in P–M systems took about 3 weeks, although their physical characteristics only lasted about 2 weeks. Correlations among ambient densities and adjacent P–M systems were mixed, but suggested decoupling between local ambient and P–M dynamics for some taxa either in relation to age of the patch and/or size of the individuals. At the community level, local differences appeared to be a significant source of variation in new pits, but differences were swamped out when recruitment was high. Differences were more evident in older P–M systems. These results show that sources of local variation in infaunal dynamics can be attributed to a combination of small-scale disturbance/recovery processes and spatially and temporally changing ambient conditions. Identifying extant spatial and temporal small-scale variation can be a critical component of understanding and interpreting larger-scale dynamics of soft-sediment systems.