Seasonal dynamics of microzooplankton communities in the Sea of Oman (Arabian Sea)

Authors

  • N. Aberle Norwegian University of Science and Technology, Department of Biology, Trondheim Biological Station, 7491 Trondhjem, Norway
  • S.A. Piontkovski Sultan Qaboos University, College of Agricultural and Marine Sciences, Dept. of Marine Sciences and Fisheries, P.O. Box 34 123 Al-Khoud, Sultanate of Oman

Keywords:

protozoa, protozooplankton, nauplii, appendicularia, Noctiluca, tintinnid

Abstract

Seasonal dynamics of microzooplankton and changes in environmental condition were analysed during a one-year field sampling campaign in the Sea of Oman at two different stations. Monsoon winds in this region cause distinct seasonality patterns with high primary productivity during the south-west monsoon in summer (June to October) and north-east monsoon periods in winter (November to March). Microzooplankton in the Sea of Oman showed several biomass peaks throughout the year. In general, higher biomass occurred during the south-west monsoon when compared to the north-east monsoon period with maxima of 190 µg C l−1at the inshore station Bandar Al-Khyran at 1m and 308 µg C l−1 at 10m water depth. At the offshore-station, peaks of 372 µg C l−1 (1m) and 256 µg C l−1 (20m) occurred during the south-west monsoon. A strong coupling between phytoplankton and microzooplankton was observed during monsoon periods but some microzooplankton peaked during inter-monsoon periods when chlorophyll concentration was low (Bandar Al-Khyran: 372 µg C l−1 at 1m and 196 µg C l−1, 10m; Offshore-station: 419 µg C l−1, 20 m). The initiation of phytoplankton blooms in the Sea of Oman was bottom-up controlled due to strong seasonal nutrient influx during south-west and north-east monsoon periods. Highest microzooplankton biomass occurred during monsoon periods with a dominance of Noctiluciphyceae and peaks of 7596 µg C l−1 at Bandar Al-Khyran (1m) and 5942 µg C l−1 (10m). Copepod nauplii, Amoebozoa and Larvacea contributed substantially to microzooplankton biomass throughout the year. Ciliophora contributed low proportion to the total microzooplankton biomass peaking both during monsoon and inter-monsoon periods. During the spring inter-monsoon, choreotrich ciliates (tintinnids) showed distinct peaks of 15.9 µg C l−1 at Bandar Al-Khyran (1m) and 17.7 µg C l−1 (10m) as well as 18.2 µg C l−1 at Offshore-station (20m). The interplay between bottom-up controlled primary production and top-down control mechanisms regulates the phenology patterns of specific microzooplankton groups in the Sea of Oman thus pointing at complex trophodynamic interactions at the lowermost foodweb level in this low-latitude ecosystem.

References

Aberle, N.

, Lengfellner, K.

, Sommer, U.

, 2007. Spring bloom succession, grazing impact and herbivore selectivity of ciliate communities in response to winter warming. Oecologia 150, 668–681.

Aberle, N.

, Malzahn, A.M.

, Lewandowska, A.

, Sommer, U.

, 2015. Some like it hot: the microzooplankton-copepod link in a warming ocean. Mar. Ecol. Prog. Ser. 519, 103–113.

Al-Azri, A.R.N.

, Piontkovski, S.A.

, Al-Hashmi, K.A.

, Goes, J.I.

, do Gomes, H.R.

, 2010. Chlorophyll a as a measure of seasonal coupling between phytoplankton and the monsoon periods in the Gulf of Oman. Aquat. Ecol. 44, 449–461.

Al-Azri, A.

, Piontkovski, S.

, Al-Hashmi, K.

, Al-Gheilani, H.

, Al-Habsi, H.

, Al-Khusaibi, S.

, Al-Azri, N.

, 2012. The occurrence of algal blooms in Omani coastal waters. Aquat Ecosyst. Health Mgmt. 15(1), 56–63.

Al-Hashmi, K.

, Goes, J.I.

, Claereboudt, M.

, Piontkovski, S.

, Al Azri, A.

, Smith, S.L.

, 2014. Variability of dinoflagellates and diatoms in the surface waters of Muscat, Sea of Oman: comparison between enclosed and open ecosystem. Int J Ocean Oceanogr. 8, 137–152.

Azam, F.

, Fenchel, T.

, Field, J.G.

, Gray, J.S.

, Meyer-Reil, L.A.

, Thingstad, F.

, 1983. The ecological role of water-column microbes in the sea. Mar. Ecol. Prog. Ser. 10, 257–263.

Bils, F.

, Moyano, M.

, Aberle, N.

, Hufnagl, M.

, Alvarez-Fernandez, S.

, Peck, M.A.

, 2017. Exploring the microzooplankton-ichthyoplankton link: a combined field and modeling study of Atlantic herring (Clupea harengus) in the Irish Sea. J. Plankton Res. 39, 147–163.

Boyce, D.G.

, Lewis, M.R.

, Worm, B.

, 2010. Global phytoplankton decline over the past century. Nature 466, 591–596.

Burkill, P.H.

, Mantoura, R.F.C.

, Owens, N.J.P.

, 1993. Biogeochemical cycling in the Northwestern Indian Ocean - A brief overview. Deep-Sea Res. 40, 643–649.

Calbet, A.

, 2008. The trophic roles of microzooplankton in marine systems. ICES J. Mar. Sci. 65, 325–331.

Dennett, M.R.

, Caron, D.A.

, Murzov, S.A.

, Polikarpov, I.G.

, Gavrilova, N.A.

, Georgieva, L.V.

, Kuzmenko, L.V.

, 1999. Abundance and biomass of nano- and microplankton during the 1995 Northeast Monsoon and Spring Intermonsoon in the Arabian Sea. Deep-Sea Res. 46, 1691–1717.

Figueiredo, G.M.

, Montagnes, D.J.S.

, Nash, R.D.M.

, 2009. The importance of protozooplankton as prey for copepods in the coastal areas of the central Irish Sea. Hydrobiologia 628, 227–239.

Gifford, D.J.

, Caron, D.A.

, 2000. Sampling, preservation, enumeration and biomass of marine protozooplankton. In:

Roger Harris

,

J. Lenz

,

M. Huntley

,

P. Wiebe

,

H.R. Skjoldal

(Eds.),

ICES Zooplankton Methodology Manual

, pp. 193–221. Academic Press, MA.

Goes, J.I.

, Thoppil, P.G.

, Gomes, H.D.

, Fasullo, J.T.

, 2005. Warming of the Eurasian landmass is making the Arabian Sea more productive. Science 308, 545–547.

Gowing, M.M.

, Garrison, D.L.

, Wishner, K.F.

, Gelfman, C.

, 2003. Mesopelagic microplankton of the Arabian Sea. Deep-Sea Research Part 50, 1205–1234.

Hopcroft, R.R.

, Roff, J.C.

, 1998. Zooplankton growth rates: the influence of size in nauplii of tropical marine copepods. Mar. Biol. 132, 87–96.

Hopcroft, R.R.

, Roff, J.C.

, Lombard, D.

, 1998. Production of tropical copepods in Kingston Harbour, Jamaica: the importance of small species. Mar. Biol. 130, 593–604.

Irigoien, X.

, Flynn, K.J.

, Harris, R.P.

, 2005. Phytoplankton blooms: a 'loophole' in microzooplankton grazing impact? J. Plankton Res. 27, 313–321.

Jaspers, C.

, Nielsen, T.G.

, Carstensen, J.

, Hopcroft, R.R.

, Moller, E.F.

, 2009. Metazooplankton distribution across the Southern Indian Ocean with emphasis on the role of Larvaceans. J. Plankton Res. 31, 525–540.

Jonasdottir, S.H.

, Nielsen, T.G.

, Borg, C.M.A.

, Moller, E.F.

, Jakobsen, H.H.

, Satapoomin, S.

, 2013. Biological oceanography across the Southern Indian Ocean - basin scale trends in the zooplankton community. Deep-Sea Res 75, 16–27.

Landry, M.R.

, Calbet, A.

, 2004. Microzooplankton production in the oceans. ICES J. Mar. Sci. 61, 501–507.

Loeder, M.G.J.

, Kraberg, A.C.

, Aberle, N.

, Peters, S.

, Wiltshire, K.H.

, 2012. Dinoflagellates and ciliates at Helgoland Roads, North Sea. Helgol. Mar. Res. 66, 11–23.

Lopez-Urrutia, A.

, Irigoien, X.

, Acuna, J.L.

, Harris, R.

, 2003. In situ feeding physiology and grazing impact of the appendicularian community in temperate waters. Mar. Ecol. Prog. Ser. 252, 125–141.

Montagnes, D.J.S.

, Dower, J.F.

, Figueiredo, G.M.

, 2010. The Protozooplankton-Ichthyoplankton Trophic Link: An Overlooked Aspect of Aquatic Food Webs. J. Eukaryot Microbiol. 57, 223–228.

Piontkovski, S.

, Chiffings, T.

, 2014. Long-term changes of temperature in the Sea of Oman and the Western Arabian Sea. Int. J. Ocean Oceanogr. 8, 53–72.

Piontkovski, S.A.

, Claereboudt, M.R.

, 2012. Interannual changes of the Arabian Sea productivity. Mar Biol Res 8, 189–194.

Piontkovski, S.A.

, Al-Azri, A.R.N.

, Al-Hashmi, K.A.

, 2011. Seasonal and interannual variability in chlorophyll a in the Gulf of Oman compared to the open Arabian Sea regions. Int. J. Remote Sens. 32, 7703–7715.

Piontkovski, S.

, Al-Maawali, A.

, Al-Muna Al-Manthri, W.

, Al-Hashmi, K.

, Popova, E.

, 2013. Zooplankton of Oman coastal waters. Agricult. Mar. Sci. 18, 37–50.

Rao, S.A.

, Dhakate, A.R.

, Saha, S.K.

, Mahapatra, S.

, Chaudhari, H.S.

, Pokhrel, S.

, Sahu, S.K.

, 2012. Why is Indian Ocean warming consistently? Clim. Chang. 110, 709–719.

Richardson, A.J.

, 2008. In hot water: zooplankton and climate change. ICES J Mar Sci 65, 279–295.

Rose, J.M.

, Caron, D.A.

, 2007. Does low temperature constrain the growth rates of heterotrophic protists? Evidence and implications for algal blooms in cold waters. Limnol. Oceanogr. 52, 886–895.

Sherr, E.B.

, Sherr, B.F.

, Paffenhoefer, G.A.

, 1986. Phagotrophic protozoa as food for metazoans: A "missing" trophic link in marine pelagic food webs? Mar. Microb. Food Webs 1, 61–80.

Skalar

, 1996. Skalar Analytical Manual, Segmented flow analyser, Publication No. 0101022A.

Sommer, F.

, Hansen, T.

, Feuchtmayr, H.

, Santer, B.

, Tokle, N.

, Sommer, U.

, 2003. Do calanoid copepods suppress appendicularians in the coastal ocean? J. Plankton Res. 25, 869–871.

Strickland, J.

, Parsons, T.

, 1972. A practical handbook of sea water analysis. Fisheries Research Board of Canada, Ottawa, ON.

Published

2019-04-03