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Fragilariopsis Sp. Bloom Causes Yellowish-Brown Waters Off Alappuzha, South-Central Kerala Coast, India, during the Mud Bank-Upwelling Phase


Affiliations
1 CSIR-National Institute of Oceanography, Regional Centre, Kochi 682 018, India
2 CSIR-National Institute of Oceanography, Dona Paula, Goa 403 004, India
 

Mud banks (Chakara) of Kerala are calm coastal waters that form in several isolated stretches along the coast usually during the southwest monsoon (SWM) period (June–September). They are characterized by the damping of incident waves, generating localized calm sea environment conducive for fishing activities, while the high monsoon waves create hostile environment in the rest of the region. Here, we present the scientific basis of the yellowish-brown discoloration of water column that occurs off Alappuzha, Kerala annually during the peak and late SWM associated with coastal upwelling-mud bank event. The discoloured waters that occur off Alappuzha associated with these events are locally known as ‘pola vellam’, which is nothing but diatom blooms. In 2014, pola vellam was actually caused by the bloom of Fragilariopsis (= Fragilaria) sp.; hereafter Fragilariopsis, which was widespread in the study region, even beyond the mud bank domain. This bloom feature is attributable to the nutrient enrichment associated with intense coastal upwelling that was dominant over a larger spatial extent in the study domain, including the mud bank. FlowCAM-based plankton data strongly support the above view, as the abundance, biovolume and biomass of Fragilariopsis had similar temporal trend both in the mud bank and non-mud bank regions. The general ecology and importance of Fragilariopsis bloom in the study domain, from the point of view of commercial fisheries, is also elaborated in this communication.

Keywords

Bloom, Coastal Upwelling, Fragilariopsis sp., Mud Bank, Fisheries.
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  • Damodaran, R., Meio-benthos of the mud banks of Kerala coast. Proc. Indian Acad. Sci., Sect. B, 1972, 38, 288–297.
  • Silas, E. G., Mud banks of Kerala–Karnataka: need for integrated study. CMFRI Bull., 1984, 31, 2–7.
  • Regunathan, A., Mathew, K. J., Kurup, N. S. and Murty, A. V. S., Monsoon fishery and mud banks of Kerala coast. CMFRI Bull., 1981, 30, 37–41.
  • Regunathan, A., Mathew, K. J., Rao, D. S., Gopinathan, C. P., Kurian, N. P. and Murty, A. V. S., Fish and fisheries of the mudbanks. CMFRI Bull., 1984, 31, 60–71.
  • Karnan, C., Jyothibabu, R., Arunpandi, N., Jagadeesan, L., Prathihari, A., Balachandran, K. K. and Naqvi, S. W. A., Discriminating the role of coastal upwelling and mud bank in structuring the plankton size and lower level food web along the southwest coast of India. J. Mar. Syst., 2017, 172, 24–42.
  • Jyothibabu, R., Balachandran, K. K., Jagadeesan, L., Karnan, C., Arunpandi, N., Naqvi, S. W. A. and Pandiyarajan, R. S., Mud bank along the southwest coast of India are not too muddy for plankton. Sci. Rep., 2018, 8, 2544.
  • Murty, A. V. S., Rao, D. S., Reghunathan, A., Gopinathan, C. P. and Mathew, K. J., Ecology of mud banks-hypothesis on mud banks. CMFRI Bull., 1984, 31, 8–20.
  • Banse, K., On the upwelling and bottom trawling off the south-west coast of India. J. Mar. Biol. Assoc. India, 1959, 1, 33–49.
  • Banse, K., Hydrography of the Arabian Sea shelf of India and Pakistan and effects on demersal fishes. Deep-Sea Res. I, 1968, 15, 45–79.
  • Nair, S. R. S., Devassy, V. P. and Madhupratap, M., Blooms of phytoplankton along the west coast of India associated with nutrient enrichment and the response of zooplankton. In Marine Coastal Eutrophication. The Response of Marine Transitional Systems to Human Impact: Problems and Perspectives for Restoration (eds Vollenweider, R. A., Marchetti, R., Viviani, R.), Elsevier, Amsterdam, The Netherlands, 1992, pp. 819–828.
  • Madhupratap, M., Shetye, S. R., Nair, K. N. V. and Nair, S. R. S., Oil sardine and Indian mackerel: their fishery, problems and coastal oceanography. Curr. Sci., 1994, 66, 340–348.
  • Jyothibabu, R. et al., The response of microzooplankton (20–200 μm) to coastal upwelling and summer stratification in the southeastern Arabian Sea. Cont. Shelf Res., 2008, 28, 653–671.
  • Jyothibabu, R., Madhu, N. V., Habeebrehman, H., Jayalakshmy, K. V., Nair, K. K. C. and Achuthankutty, C. T., Re-evaluation of ‘paradox of mesozooplankton’ in the eastern Arabian Sea based on ship and satellite observations. J. Mar. Syst., 2010, 81, 235–251.
  • Mann, K. H., Physical oceanography, food chains, and fish stocks: a review. ICES J. Mar. Sci., 1993, 50, 105–119.
  • Cury, P., Bakun, A., Crawford, R. J. M., Jarre, A., Quinones, R. A., Shannon, L. J. and Verheye, H. M., Small pelagic in upwelling systems: patterns of interaction and structural changes in ‘wasp-waist’ ecosystems. ICES J. Mar. Sci., 2000, 57, 603–618.
  • Grasshoff, K., In Methods of Seawater Analysis (eds Grasshoff, K., Ehrhardt, M. and Kremling, K.), Verlag Chemie, Weinheim, 1983, p. 419.
  • United Nations Educational, Scientific and Cultural Organization (UNESCO), Protocols for the Joint Global Ocean Flux Study (JGOFS). Core measurements. UNESCO, Paris, 29, 1994, p. 170.
  • Sieracki, C. K., Sieracki, M. E. and Yentsch, C. S., An imaging-in-flow system for automated analysis of marine microplankton. Mar. Ecol. Prog. Ser., 1998, 168, 285–296.
  • Le Bourg, B., Cornet-Barthaux, V. R., Pagano, M. and Blanchot, J., FlowCAM as a tool for studying small (80–1000 μm) metazoo-plankton communities. J. Plankton Res., 2015, 37, 666–670.
  • Mauchline, J., Blaxter, J. H. S. and Tyler, P. A., The biology of calanoid copepods. In Advances in Marine Biology, Academic Press, San Diego, CA. USA, 1998, vol. 33, p. 710.
  • Karnan, C., Jyothibabu, R., Manoj Kumar, T. M., Jagadeesan, L. and Arunpandi, N., On the accuracy of assessing copepod size and biovolume using FlowCAM and traditional microscopy. Indian J. Geo-Mar. Sci., 2017, 46, 1261–1264.
  • Zachariah, P. U. and Abdurahiman, K. P., Methods of stomach content analyses of fishes – building mass balance trophic and simulation models. Technical Notes, Central Marine Fisheries Research Institute (CMFRI), Kochi, 2004, p. 200.
  • Nair, R. V. and Subrahmanyan, R., The diatom, Fragilaria oceanica Cleve, an indicator of abundance of the Indian oil sardine, Sardinella longiceps Cuv. and Val. Curr. Sci., 1955, 24, 41–42.
  • Takabayashi, M., Lew, K., Johnson, A., Marchi, A. L., Dugdale, R. and Wilkerson, F. P., The effect of nutrient availability and temperature on chain length of the diatom, Skeletonema coastatum. J. Plankton Res., 2006, 28, 831–840.
  • Subrahmanyan, R., Studies on the phytoplankton of the west coast of India. Proc. Indian Acad. Sci., Sect. B, 1959, 4, 189–252.
  • Devassy, V. P., Observations on the bloom of a diatom Fragilaria oceanica Cleve. Mahasagar, 1974, 7, 101–105.
  • Tomas, C. R., Identifying Marine Phytoplankton, Academic Press/Harcourt Brace, San Diego, CA, USA, 1997, p. 858.

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  • Fragilariopsis Sp. Bloom Causes Yellowish-Brown Waters Off Alappuzha, South-Central Kerala Coast, India, during the Mud Bank-Upwelling Phase

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Authors

R. Jyothibabu
CSIR-National Institute of Oceanography, Regional Centre, Kochi 682 018, India
N. Arunpandi
CSIR-National Institute of Oceanography, Regional Centre, Kochi 682 018, India
C. Karnan
CSIR-National Institute of Oceanography, Regional Centre, Kochi 682 018, India
L. Jagadeesan
CSIR-National Institute of Oceanography, Regional Centre, Kochi 682 018, India
T. M. Manojkumar
CSIR-National Institute of Oceanography, Regional Centre, Kochi 682 018, India
K. K. Balachandran
CSIR-National Institute of Oceanography, Regional Centre, Kochi 682 018, India
S. W. A. Naqvi
CSIR-National Institute of Oceanography, Dona Paula, Goa 403 004, India

Abstract


Mud banks (Chakara) of Kerala are calm coastal waters that form in several isolated stretches along the coast usually during the southwest monsoon (SWM) period (June–September). They are characterized by the damping of incident waves, generating localized calm sea environment conducive for fishing activities, while the high monsoon waves create hostile environment in the rest of the region. Here, we present the scientific basis of the yellowish-brown discoloration of water column that occurs off Alappuzha, Kerala annually during the peak and late SWM associated with coastal upwelling-mud bank event. The discoloured waters that occur off Alappuzha associated with these events are locally known as ‘pola vellam’, which is nothing but diatom blooms. In 2014, pola vellam was actually caused by the bloom of Fragilariopsis (= Fragilaria) sp.; hereafter Fragilariopsis, which was widespread in the study region, even beyond the mud bank domain. This bloom feature is attributable to the nutrient enrichment associated with intense coastal upwelling that was dominant over a larger spatial extent in the study domain, including the mud bank. FlowCAM-based plankton data strongly support the above view, as the abundance, biovolume and biomass of Fragilariopsis had similar temporal trend both in the mud bank and non-mud bank regions. The general ecology and importance of Fragilariopsis bloom in the study domain, from the point of view of commercial fisheries, is also elaborated in this communication.

Keywords


Bloom, Coastal Upwelling, Fragilariopsis sp., Mud Bank, Fisheries.

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DOI: https://doi.org/10.18520/cs%2Fv115%2Fi1%2F152-159