Plankton concentrations near discontinuities in the water column (clines) are believed to be important for intensifying trophic interactions; however, evidence for increased feeding by predators at clines in situ is scarce. Here we demonstrate enhanced feeding near pycnoclines by a voracious planktivore, the ctenophore Mnemiopsis leidyi. To determine their feeding relative to stratification, we quantified temperature, salinity, dissolved oxygen concentration (DO), densities of ctenophores and copepods at 1 to 2 m depth intervals, and gut contents of ctenophores collected by depth layer at stations in a tributary and in the mainstem Chesapeake Bay during summer from 1999 to 2001. We tested the null hypotheses that patterns in the tributary and the bay were similar and that ctenophore vertical distributions and feeding were independent of the vertical distributions of the physical variables, stratification, and copepods. We rejected all null hypotheses. Ctenophores and copepods had peak densities below the pycnocline in the weakly stratified tributary, where DO was above 2 mg l −1 throughout the water column; by contrast, they were more concentrated above the strong pycnocline and near-anoxic waters at ~11 m in the bay. Predation on copepods by ctenophores was highest where both populations were concentrated. Our results illustrate the importance of stratification to planktonic trophic interactions for M. leidyi, which thrives in anthropogenically degraded waters and now is established throughout European seas, where it can negatively affect planktonic food webs and fisheries.KEY WORDS: Jellyfish · Aggregation · Cline · Acartia · Zooplankton · Low dissolved oxygen · Feeding · Clearance · Chesapeake Bay (USA)
Resale or republication not permitted without written consent of the publisherMar Ecol Prog Ser 500: [103][104][105][106][107][108][109][110][111][112][113][114][115][116][117][118][119][120] 2014 tion of organisms and enhanced feeding at clines abounds in the laboratory (e.g. Woodson & McManus 2007); however, evidence of increased feeding in situ is rare (see Möller et al. 2012).Ctenophores, medusae, and copepods are known to accumulate at density discontinuities in the water column (Arai 1992, Graham et al. 2001, Malej et al. 2007, Jacobsen & Norrbin 2009, Frost et al. 2010. Arai (1992) concluded that Sarsia tubulosa hydromedusae behaviorally aggregate at salinity discontinuities. Similarly, hydromedusae of Nemopsis bachei remain in discontinuities created by salinity gradients with and without thin layers of algae and copepods (Frost et al. 2010). Most Aurelia spp. medusae occur at clines (Rakow & Graham 2006, Malej et al. 2007. Acartia tonsa copepods also aggregate in layers ). Thus, gelatinous predators and their prey actively aggregate at density discontinuities. Although medusae and their feeding increase at clines (Frost et al. 2010), we know of no previous studies on ctenophore feeding in situ in relation to stratification.The mesohaline Chesapeake Bay (USA) and its tributaries can have ...