Zooplankton herbivory in the Arabian Sea during and after the SW monsoon, 1994

Citation
Es. Edwards et al., Zooplankton herbivory in the Arabian Sea during and after the SW monsoon, 1994, DEEP-SEA II, 46(3-4), 1999, pp. 843-863
Citations number
41
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY
ISSN journal
09670645 → ACNP
Volume
46
Issue
3-4
Year of publication
1999
Pages
843 - 863
Database
ISI
SICI code
0967-0645(1999)46:3-4<843:ZHITAS>2.0.ZU;2-1
Abstract
Microzooplankton herbivory in the Arabian Sea was measured using dilution e xperiments towards the end of the SW monsoon in September and during the in termonsoon to NE monsoon period in November-December 1994, Microzooplankton grazing resulted in a turnover of phytoplankton stocks that ranged from 11 to 49% per day. This was equivalent to grazing fluxes of between 1 and 17 mg Cm-3 d(-1). Depth-integrated microzooplankton herbivory ranged between 1 61 and 415 mg Cm-2 d(-1) during the SW monsoon cruise, and between 110 and 407mg Cm-2 d(-1) during the intermonsoon period. Microzooplankton grazed be tween 4 and 60% of daily primary production, with higher percentages found during the intermonsoon season. Phytoplankton growth rates during the SW mo nsoon ranged from 0.3 to 1.8 d(-1), with lower values in upwelling waters a nd higher values in downwelling and oligotrophic areas. During the intermon soon period, phytoplankton growth was more uniform across the basin and ave raged 0.68 +/- 0.15 d(-1). Microzooplankton abundance in experimental sampl es varied between 2800 and 16 162 cells l(-1), equivalent to a biomass of b etween 1.1 and 7.2 mg Cm-3. The mean cell carbon content of microzooplankto n was similar in both periods and ranged from 0.33 to 0.55 ng C cell(-1). M icrozooplankton were smallest in downwelling waters and largest in oligotro phic waters. Average clearance rates in those taxa that took up fluorescent ly-labelled algae ranged from 0.2 to 14 mu lind(-1) hr(-1). Average mesozoo plankton grazing rates, derived from biomass data, varied from 19 to 92 mg Cm-2 d(-1); these rates accounted for removal of between 4 and 12% of the d aily primary production. Mesozooplankton herbivory was most pronounced in u pwelling and downwelling waters and reduced in stratified oligotrophic wate rs during the SW monsoon period. Microzooplankton herbivory was greater tha n the average mesozooplankton herbivory at all stations, during both the SW monsoon and intermonsoon periods. (C) 1999 Elsevier Science Ltd. All right s reserved.