Abstract

We carried out an intensive sampling survey in ancient Lake Ohrid (Macedonia/Albania), covering all seasons, to determine total species number, relative species abundances and spatial distribution of Ostracoda. We identified 32 living species that belong to seven families (Candonidae, Ilyocyprididae, Cyprididae, Leptocytheridae, Limnocytheridae, Cytherideidae, and Darwinulidae) and 15 genera (Candona, Fabaeformiscandona, Candonopsis, Cypria, Cyclocypris, Ilyocypris, Eucypris, Prionocypris, Bradleystrandesia, Herpetocypris, Dolerocypris, Amnicythere, Paralimnocythere, Cytherissa, and Darwinula). Six additional species were identified from empty carapaces and valves. Dominant families in Lake Ohrid were Candonidae and Limnocytheridae, representing 53% and 16% of all species, respectively. Prevalence of species flocks in these two families confirms the “young” ancient status of the lake. Amnicythere displays a preference for oligo-haline to meso-haline waters, but some species are found in saline environments, which suggests Lake Ohrid has a marine history. Recent studies, however, indicate fluvial/glaciofluvial deposition at the onset of Lake Ohrid sedimentation. Candona is the most diverse genus in Lake Ohrid, represented by 12 living species. Paralimnocythere is represented by five living species and all other genera are represented by one or two species. Reports of Candona bimucronata, Ilyocypris bradyi, Eucypris virens, Eucypris sp., Prionocypris zenkeri, Bradleystrandesia reticulate, Herpetocypris sp. 2, and Dolerocypris sinensis are firsts for this lake. Living ostracodes were collected at the maximum water depth (280 m) in the lake (Candona hadzistei, C. marginatoides, C. media, C. ovalis, C. vidua, Fabaeformiscandona krstici, Cypria lacustris, C. obliqua and Amnicythere karamani). Cypria lacustris was overall the most abundant species and Cypria obliqua displayed the highest abundance at 280 m water depth. Principal environmental variables that influence ostracode distributions in Lake Ohrid are water depth and conductivity. In general, species richness, diversity and evenness were greater in waters <60 m deep, with highest values often found in the littoral zone, at depths <30 m. Candonids, however, displayed highest diversity in the sublittoral (30–50 m) and profundal (50–280 m) zones. The most frequent species encountered are taxa endemic to the lake (14 living species), which have a wide depth range (≤280 m), and display higher abundance with greater water depth. Non-endemic species were rare, limited to water depths <50 m, and were found mainly in the north part of the lake where anthropogenic pressure is high. Several cosmopolitan species were encountered for the first time, which suggests that these widespread species are new arrivals that may replace endemics as human impacts increase.

Highlights

  • Ancient lakes possess long continental archives of past climate and environmental changes and are hotspots of biodiversity and speciation dynamics for endemic taxa [1,2,3,4,5]

  • This information will improve the potential for using Ostracoda as bioindicators of climate and environment, and will help to interpret fossil species assemblages from sediment cores to be recovered by the Lake Ohrid Drilling Project

  • We found eight living species that had never been reported in the lake: Candona bimucronata, Ilyocypris bradyi, Eucypris virens, Eucypris sp., Prionocypris zenkeri, Bradleystrandesia reticulata, Herpetocypris sp. 2, and Dolerocypris sinensis

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Summary

Introduction

Ancient lakes possess long continental archives of past climate and environmental changes and are hotspots of biodiversity and speciation dynamics for endemic taxa [1,2,3,4,5]. Stankovič [14], Salemaa [15], Frogley and Preece [7], and Albrecht and Wilke [10] suggested that 33 (63%) of the 52 described ostracode species from Lake. We investigated the spatial distribution of each taxon and ostracode diversity and species richness in the lake. This information will improve the potential for using Ostracoda as bioindicators of climate and environment, and will help to interpret fossil species assemblages from sediment cores to be recovered by the Lake Ohrid Drilling Project. Spring inflows influence ostracode species distribution and ecology because they supply the cool, oxygen-rich water favored by all endemic forms in Lake Ohrid [37,38]. The Chara belt is the best studied zone and extends into the lower littoral, to about 20 m depth [10]

Sampling Survey
Results and Discussion
Ostracode Diversity
Spatial Distribution
Vertical Distribution
Wide Depth-Range Taxa
Biogeography and Anthropogenic Impact on Ostracode Distribution
Conclusions
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