Effects of shore sedimentation to tachypleus gigas (Müller, 1785) spawning activity from Malaysian waters
Ripraps, land reclamation and fishing jetty renovation were perturbing Balok Beach shores between the years 2011 and 2013 and visible impacts were scaled using horseshoe crab spawning yields. Initially, placement of ripraps at Balok Beach effectively reduced erosion and created a suitable spawning...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English English |
| Published: |
Universiti Malaysia Terengganu ( UMT )
2019
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| Subjects: | |
| Online Access: | http://irep.iium.edu.my/72618/ http://irep.iium.edu.my/72618/ http://irep.iium.edu.my/72618/1/72618_Effects%20of%20shore%20sedimentation%20to%20Tachypleus_article.pdf http://irep.iium.edu.my/72618/2/72618_Effects%20of%20shore%20sedimentation%20to%20Tachypleus_scopus.pdf |
| Summary: | Ripraps, land reclamation and fishing jetty renovation were perturbing Balok Beach shores between the years 2011 and 2013 and visible impacts were scaled using horseshoe crab
spawning yields. Initially, placement of ripraps at Balok Beach effectively reduced erosion and created a suitable spawning ground for the horseshoe crab, Tachypleus gigas. However sediments begun to gather on the beach onward year 2012 which increased shore elevation and caused complete shore surface transition into fine sand properties. This reduced sediment compaction and made Balok
Beach less favourable for horseshoe crab spawning. During the dry Southwest monsoon, Balok River estuary retains more dense saline water which assists with sediment circulation at the river mouth section. Comparatively, the less dense freshwater during the wet Northeast monsoon channels sediments shoreward. Circa-tidal action that takes place at Balok River sorts the shore sediments to
produce an elevated and steep beach. Hence, the reduced number of T. gigas nests and eggs retrieved
during year 2013 (after comparing with yield of year 2012) at Balok Beach are indicating impacts from anthropic-caused sedimentation. Models need to be constructed and associated with T. gigas spawning-migration to fully understand sediment transport especially at coastal areas that need or are undergoing nourishment. |
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