Mercury concentrations in Antarctic zooplankton with a focus on the krill species, Euphausia superba

The Antarctic is the most isolated region in the world; nevertheless, it has not avoided the negative impact of human activity, including the inflow of toxic mercury (Hg). Hg deposited in the Antarctic marine environment can be bioavailable and accumulate in the food web, reaching elevated concentrations in high-trophic-level biota, especially if methylated. Zooplankton, together with phytoplankton, are critical for the transport of pollutants, including Hg to higher trophic levels. For the Southern Ocean ecosystem, one of the key zooplankton components is the Antarctic krill Euphausia superba, the smaller euphausiid Thysanoessa macrura, and the amphipod Themisto gaudichaudii - a crucial food source for most predatory fish, birds, and mammals. The main goal of this study was to determine the Hg burden, as well as the distribution of different Hg forms, in these dominant Antarctic planktonic crustaceans. The results showed that the highest concentrations of Hg were found in T. gaudichaudii, a typically predatory taxon. Most of the Hg in the tested crustaceans was labile and potentially bioavailable for planktivorous organisms, with the most dangerous methylmercury (MeHg) accounting for an average of 16 % of the total mercury. Elevated Hg concentrations were observed close to the land, which is influenced by the proximity to penguin and pinniped colonies. In areas near the shore, volcanic activity might be a possible cause of the increase in mercury sulfide (HgS) content. The total Hg concentration increased with the trophic position and ontogenetic stage of predation, specific to adult organisms. In contrast, the proportion of MeHg decreased with age, indicating more efficient demethylation or elimination. The Hg magnification kinetics in the study area were relatively high, which may be related to climate-change induced alterations of the Antarctic ecosystem: additional food sources and reshaped trophic structure.

Autumn vertical distribution of zooplankton in the oxygen minimum zone of the Eastern Tropical North Pacific

To confirm the Habitat Compression Hypothesis, a cruise to the Eastern Tropical North Pacific (ETNP) took place at the entrance of the Gulf of California, in an area rarely studied at the southern limit of the California Current, where it mixes with waters of the West Mexican Current and the Gulf of California. No significant day-night differences in the vertical distribution (0-500 m depth) of zooplankton were found based on 22 MOCNESS tows and, for the first time, a 48-h cycle of stratified zooplankton sampling. Most zooplankton groups were observed within the upper 100 m, above the oxycline, with oxygen concentrations as low as 45 μmol kg-1. Some California Current-influenced samples showed a slightly different vertical distribution. A ∼50% reduction in the number and abundance of 24 zooplankton groups was recorded within the Oxygen Minimum Zone, from 100 to 500 m depth. Vertical migrator's exceptions include some euphausiid species that migrate into the OMZ during the day. Principal Component Analyses showed that the vertical distribution of zooplankton is limited by oxygen, with a low zooplankton carbon density below ∼100 m depth within the OMZ. The difference between day and night for the upper 0-100 m layer was non-significant (U221 = 57; p = 0.947); however, the data showed great variability. Thus, zooplankton Carbon remains relatively constant, in the upper 100 m, and is available during day and night, in the studied area.