1 Author version of : Journal of Marine Systems, vol.204; 2020; Article no: 103308 Phytoplankton associated with seasonal oxygen depletion in waters of the western continental shelf of India a, b a a a a M. Gauns *, S. Mochemadkar , A. Pratihary , G.Shirodkar , P. V. Narvekar , S.W.A. Naqvi aNational Institute of Oceanography (Council of Scientific & Industrial Research), Dona Paula, Goa, 403 004, India bDepartment of Fisheries Directorate of Fisheries, Govt.of Goa, Panaji – Goa, India *Corresponding author:
[email protected] (M. Gauns). Abstract We report here results of a time series study carried out to understand seasonal variability of phytoplankton in relation to changes in dissolved oxygen based on observations at the Candolim Time Series (CaTS) station located in coastal waters of Goa, Central West Coast of India. The water column remains well oxygenated during the non-southwest (SW) monsoon period (November-May). However, upwelling of water already depleted in dissolved oxygen during the SW monsoon, coupled with degradation of copious amounts of locally produced organic matter, leads to severe oxygen depletion including sulphate reduction beneath a thin surface layer during late summer-early autumn (August-October). The onset of oxygen-deficient conditions greatly alters the community structure of water-column phytoplankton.Pico-autotrophs and pennate diatoms were found to dominatethe autotrophic biomass in such oxygen depleted waters. Keywords: Phytoplankton, Coastal upwelling, Dissolved oxygen, Picoplankton ,West coast of India 2 1. Introduction Biological productivity in the Arabian Sea is regulated mainly by nutrient inputs from subsurface waters via upwelling in summer and convective mixing in winter (Banse and Mc Clain, 1986, Madhupratap et al., 1996;Barber et al., 2001).