Crustacean calcium bodies are epithelial sacs which contain a mineralized matrix. The objectives of this study were to describe the microscopic anatomy of calcium bodies in the terrestrial isopod Hyloniscus riparius and to establish whether they undergo molt-related structural changes. We performed 3D reconstruction of the calcium bodies from paraffin sections and analyzed their structure with light and electron microscopy. In addition, we analyzed the chemical composition of their mineralized matrices with micro-Raman spectroscopy. Two pairs of these organs are present in H. riparius. One pair is filled with bacteria while the other pair is not. In non-molting animals, the bacteria-filled calcium bodies contain apatite crystals and the bacteria-free calcium bodies enclose CaCO3-containing concretions with little organic matrix. During preparation for molt, an additional matrix layer is deposited in both pairs of calcium bodies. In the bacteria-filled calcium bodies it contains a mixture of calcium carbonate and calcium phosphate, whereas only calcium carbonate is present in bacteria-free calcium bodies. After ecdysis, all mineral components in bacteria-free calcium bodies and the additional matrix layer in bacteria-filled calcium bodies are completely resorbed. During calcium resorption, the apical surface of the calcium body epithelium is deeply folded and electron dense granules are present in spaces between epithelial cells. Our results indicate that the presence of bacteria might be linked to calcium phosphate mineralization. Calcium bodies likely provide a source of calcium and potentially phosphate for the mineralization of the new cuticle after molt. Unlike other terrestrial isopods, H. riparius does not form sternal CaCO3 deposits and the bacteria-free calcium bodies might functionally replace them in this species.
COBISS.SI-ID: 2756943
from: Elliot Shubert [e.shubert@nhm.ac.uk] Nomination for Outstanding Paper for 2013 your paper: Fiser, C., Zagmajster, M. & Ferreira, R. L. 2013. Two new amphipod Families recorded in South America shed light on an old biogeographical enigma. Systematics and Biodiversity 11(2): 117-139, was nominated for the Outstanding Paper Award for 2013. Unfortunately, it was not selected as a winner; however, it is important to know that your paper was highly rated by the editorial team. The known diversity of freshwater amphipods in South America is substantially lower than on other continents. This has puzzled biologists for decades. Two hypotheses have been proposed in attempts to explain this pattern. According to the first one, the majority of amphipod lineages never dispersed across South America. The alternative hypothesis is that the recently diversified hyalellids have outcompeted and depleted the ancestral amphipod fauna. The recently discovered freshwater amphipod species Seborgia potiguar sp. nov. (Seborgidae) and Potiberaba porakuara gen. nov., sp. nov. (Mesogammaridae) from Brazil reveals the existence of two additional families of amphipods in South America. In the light of these discoveries we have analysed the amphipod faunistic structure of South America to test the above two biogeographic hypotheses. First, the number of amphipod families in South America is not as low as was thought. Falklandellididae are limited to the Falkland Islands and Chile. All other families (Ingolfiellidae, Bogidiellidae, Phreatogammaridae, Paraleptamphopidae, Pseudoingolfiellidae, Paracorpohiinae, Mesogammaridae and Seborgidae) but one (Dogielinotidae) share two properties: (1) they have a transoceanic distribution and (2) they are from subterranean waters. Since the dispersal ability of amphipods is limited, trans-oceanic disjunctions are best explained by plate tectonics, which implies their early origin, negating the first biogeographical hypothesis. These ancient families, for unknown reasons, survived only in a stable subterranean environment which can be regarded as a refuge. The only recent colonizer of the continent might be Dogielinotidae with the species-rich genus Hyalella. Although it cannot be determined whether hyallelids truly out-competed ancient amphipods, we suggest that the second hypothesis fits better to the data. Further findings of amphipods are expected in South America, especially from subterranean waters. This habitat is highly endangered in Brazil, and should be more rigorously protected.
COBISS.SI-ID: 2819663
Like most other cave animals, the Proteus anguinus anguinus (cave-dwelling salamander) experiences periodically with poor and discontinuous food supply and/or intermittent hypoxia that may occur for long periods in the subterranean environments. Proteus adjusts its metabolism and utilization of metabolic reserves to these fluctuating periods of food supply. In this research we studied morphological and biochemical changes of liver tissue of the cave-dwelling salamander during periods of food deprivation. With a combination of qualitative morphological and quantitative biochemical data we evaluate the adaptive capacity of the liver and the importance of the liver as an energy storing organ.
COBISS.SI-ID: 2779983
The Gammaridae shows the greatest disparity in species diversity and distribution pattern in the Amphipoda, with some genera ranging from the Palearctic to Nearctic, while others are limited to the Mediterranean region or ancient Tethyan margins. Here we present the first molecular phylogenetic analysis of the Gammaridae to investigate its evolutionary history using four genetic markers and a comprehensive set of taxa representing 198 species. The phylogenetic results revealed that the Gammaridae originated from the Tethyan region in the Cretaceous, and split into three morphologically and geographically distinct lineages by the end of the Paleocene. Diversification analysis combined with paleogeological evidence suggested that the Tethyan changes induced by sea-level fluctuation and tectonic uplift triggered different diversification modes and range expansions for the three lineages. The Gammarus lineage underwent an early rapid radiation across Eurasia and North America, then declined towards modern species. Pontogammarids maintained stable diversification with restricted distributions around the Tethyan basin, whereas sarothrogammarids experienced evolutionary stasis by stranding on the ancient Tethyan margins. Our findings suggest that environmental changes have played an important role in the diversification of Gammaridae lineages, which could be an opportunity to promote adaptive radiations in new habitats, or constraints resulting in evolutionary relicts.
COBISS.SI-ID: 2936399
The Vjetrenica cave in the Dinaric Karst hosts a worldwide extraordinarily high cave biodiversity. Beside a diverse and specialized cave fauna, sprout-like formations attached to the bed of the cave stream were observed and described, but not further characterized, almost a century ago. Here we investigated these sprout-like microbial aggregates by the rRNA approach and detailed microscopy. Based on fluorescence in situ hybridization and ultrastructural analysis, the sprout-like formations are morphologically highly organized, and their core consists of a member of a novel deep-branching lineage in the bacterial phylum Nitrospirae. This organism displays an interesting cellular ultrastructure with different kinds of cytoplasmic inclusions and is embedded in a thick extracellular matrix, which contributes to the stability and shape of the aggregates. This novel bacteriumhas been provisionally classified as Candidatus Troglogloea absoloni. The surface of the sprout-like aggregates is more diverse than the core. It is colonized by a bacterial biofilm consisting primarily of filamentous Betaproteobacteria, whereas other microbial populations present inthe crust include members of the Bacteriodetes, Gammaproteobacteria, Actinombacteria, Alphaproteobacteria, and Planctomycetes, which are intermingled with mineral inclusions. This study represents the first thorough molecular and ultrastructural characterization of the elusive sprout-like bacterial aggregates, which are also found in other cave systems of the Dinaric Karst. The discovery of Ca. Troglogloea absoloni contributes tothe known biodiversity of subterranean ecosystems and especially of macroscopic structures formed in caves by microorganisms, whose composition and ecological function often remain enigmatic.
COBISS.SI-ID: 2711375