IMIS | Flanders Marine Institute
 

Flanders Marine Institute

Platform for marine research

IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Printer-friendly version

Biogenic sedimentary structures on a Korean mud flat: spring-neap variations
Lee, Y.-H.; Koh, C.-H. (1994). Biogenic sedimentary structures on a Korean mud flat: spring-neap variations. Neth. J. Sea Res. 32(1): 81-90
In: Netherlands Journal of Sea Research. Netherlands Institute for Sea Research (NIOZ): Groningen; Den Burg. ISSN 0077-7579, more
Peer reviewed article  

Available in Authors 

Keyword
    Marine

Authors  Top 
  • Lee, Y.-H.
  • Koh, C.-H.

Abstract
    Biogenic sedimentary structures created by dominant benthic animals of a mud flat were investigated in a small embayment at Panweol on the west coast of Korea. Burrows were replicated using the resin casting method on a sufficiently large scale to evaluate their variations statistically. The size and shape of burrows and other traces varied with locations and tidal phases. Burrows of the upper-intertidal crabs Helice tridens sheni and Ilyoplax dentimerosa were T- or I-shaped, vertical and deep, whereas those of the mid-intertidal crab Macrophthalmus japonicus were U-shaped, oblique and shallow. The upper-intertidal polychaete Perinereis aibuhitensis, a subsurface feeder, had sinuous and highly-branched burrows while the mid-intertidal one Periserrula leucophryna, a surface feeder, had vertical burrows without subsurface branches. Variations of crab burrows with tidal phases were distinct: The burrows of both H. tridens sheni and M. japonicus were significantly deeper and wider during neap tides than during spring tides. Sediment mounds were common in the upper intertidal zone, while crawling and feeding traces such as trails, trackways and cheliped scrapings were more prominent in the mid-intertidal zone. These traces were also observed in the upper intertidal zone during spring tides when surface sediments became watery. The size of the sediment mounds varied, being largest during neap tides. These biogenic sedimentary structures observed at Panweol were distinctly different from those found near Inchon only 50 km away, probably due to differences in hydrology and sedimentology.

All data in IMIS is subject to the VLIZ privacy policy Top | Authors