Seasonal variation in erodibility of two temperate, microtidal mudflats

Authors
Citation
Tj. Andersen, Seasonal variation in erodibility of two temperate, microtidal mudflats, EST COAST S, 53(1), 2001, pp. 1-12
Citations number
33
Categorie Soggetti
Aquatic Sciences
Journal title
ESTUARINE COASTAL AND SHELF SCIENCE
ISSN journal
02727714 → ACNP
Volume
53
Issue
1
Year of publication
2001
Pages
1 - 12
Database
ISI
SICI code
0272-7714(200107)53:1<1:SVIEOT>2.0.ZU;2-6
Abstract
The erodibility of two microtidal mudflats in the Danish Wadden Sea area wa s examined over a year at monthly intervals (EROMES erosion equipment). One site was dominated by macrofauna (mainly Hydrobia ulvae) whereas the other was only sparsely inhabited by macrofauna with the temporary formation of diatom biofilms. The erodibility of the mudflat surface was mediated by the presence of both biofilms and H. ulvae. Biofilms increase erosion threshol d and decrease the erosion rate but the correlation between chlorophyll a a nd erosion threshold was not strong. Biofilms formed in spring, summer and autumn at one study site and the erodibility of the site was consequently g enerally low during these seasons and higher during the winter period. Biof ilms were absent where macro faunal populations were dominant and low erosi on thresholds were found at these sites. The erosion rate was dependent on the fecal pellet content of the bed material. A strong seasonal variation o f the content of fecal pellets of the bed material was found and this cause s a seasonal variation of the erosion rate. The temporal variation of the e rodibility at the sites dominated by H. ulvae was actually opposite to the other sites as an increase in the erosion rate was observed during the warm er seasons, probably due to the higher egestion-rate and higher production of fecal pellets by H. ulvae under higher temperatures. The data demonstrat es that sites dominated by H. ulvae are easily eroded, both because of the snails grazing activities on benthic diatoms and the pelletization of the s urface material. However, it is only by examination of the erosion rates in addition to the erosion thresholds that the destabilizing effect of H. ulv ae becomes clear. The study demonstrates that the prediction of the seasona lity of the erodibility at intertidal mudflats is not straightforward but r equires information on both benthic micro algae contents and macrofaunal co mmunity structure and population densities. (C) 2001 Academic Press.