Influence of upwelling induced near shore hypoxia on the Alappuzha mud banks, South West Coast of India. (1st May 2017)

• Record Type: Journal Article
• Authors: Gireeshkumar, T.R.; Mathew, D.; Pratihary, A.K.; Naik, H.; Narvekar, K.U.; Araujo, J.; Balachandran, K.K.; Muraleedharan, K.R.; Thorat, B.; Nair, M.; Naqvi, S.W.A.
• Is Part Of: Continental shelf research. Volume 139(2017)
• Page Start: 1
• Page End: 8
• Publication Date: 2017-05-01
• Subjects: Upwelling -- Mud banks -- Hypoxia -- Nutrients -- Fish availability -- Arabian Sea; Continental shelf -- Periodicals; Submarine geology -- Periodicals; 551.41
• DOI: 10.1016/j.csr.2017.03.009
• Languages: English
• ISSNs: 0278-4343

Abstract

Abstract: The results of the first time-series measurements spanning 18-weeks (22 April to 20 September 2014) from a coastal environment (Alappuzha, southwest India), where two process of upwelling and mud banks are concurrent during summer monsoon are presented. The upwelling signals were evident from the 2nd week of May onwards and the intensity varied widely from 1st week of June to 3rd week of September. The formation of mud banks was observed during the peak upwelling period (14th June) and once formed, they were persistent till the end of monsoon season (September 2014). The time-series evolution of dissolved oxygen levels showed the incursion of hypoxic waters well in to the mud banks during peak upwelling period. The considerable reduction in the dissolved methane levels (300 to <50 nM) during hypoxia is an anomaly, which may be due to some microbial processes. The incursion of hypoxic waters in to the Alappuzha mud banks is the first observation and is significant because, it can now explain why mud banks are not always good fishing grounds. The present study shows that the fish availability is mainly dependent on the incursion and prevalence of hypoxic waters in the mud banks. Highlights: The response of the mud banks to the monsoon upwelling is delineated. Upwelling created hypoxic/suboxic conditions in the mud bank region (even at 3 m). The hypoxic areas experienced denitrification, evidenced by the nitrogen deficit. Dissolved methane showed a progressive decrease with the intensification of hypoxia.