Morphology and function of the hyoid apparatus of fossil xenarthrans (mammalia)

The analysis of the hyoid apparatus of fossil xenarthrans provides insight on the form of the tongue and its function in food intake and intraoral processing. The hyoid apparatus of xenarthrans is notable for fusion among its elements. The presence of a V‐bone, a complex consisting of fused basihyal and thyrohyal bones, is a consistent and probably synapomorphic feature of xenarthrans. Fusion of other elements is variable in fossil xenarthrans. Most fossil sloths retain independent elements, as in living dasypodids and mammals generally. Among nothrotheriids, the elements are slender and their articular surfaces indicate considerable mobility, and the relatively long and horizontal orientation of the geniohyoid muscle suggests considerable tongue protrusion. Among mylodontines, such as Paramylodon and Glossotherium, the elements indicate relatively mobile articulations, except between the stylo‐ and epihyals. The relatively posterior placement of the apparatus and the length and alignment of the geniohyoid muscle indicate considerable capacity for tongue protrusion. Scelidotherium, however, had rigidly articulated stylohyal and epihyal, and the apparatus lies farther anteriorly, which together with the elongated, steeply inclined mandibular symphysis, indicates a relatively shorter geniohyoid muscle and thus more limited capacity for tongue protrusion. A similar situation is indicated for Megatherium, casting doubt on the classical reconstruction of this sloth as having a long prehensile tongue. Among cingulates Prozaedyus resembles living dasypodids, indicating considerable tongue protrusion important in food acquisition and intake. More extensive fusion of hyoid elements occurs in the cingulates Glyptodon and Proeutatus, in which the stylohyal and epihyal at least, are fused into a single element termed the sigmohyal. The presence of this element supports recent proposals of a sister‐group relationship between glyptodonts and eutatines. The rigidity of the apparatus suggests limited tongue protrusion, but the tongue, in glyptodonts at least, was a powerful structure important for intraoral manipulation of food. J. Morphol. 271:1119–1133, 2010. © 2010 Wiley‐Liss, Inc.     

Invertebrate Biodiversity in Antarctic Dry Valley Soils and Sediments

We studied invertebrate communities across a transition zone between soils and stream sediments in the cold desert landscape of Taylor Valley, Antarctica. We hypothesized that hydrological and biogeochemical linkages in the functionally important transition zone between streams and surrounding soils should be important in structuring invertebrate communities. We compared invertebrate communities along transects beginning in the saturated sediments under flowing stream water and extending laterally through the hyporheic zone to the dry soils that characterize most of the dry valley landscape. Nematodes, rotifers, and tardigrades assembled into different communities in soils and sediments, but there was no relationship between the total abundance of invertebrates and moisture. Community diversity was, however, influenced by the moisture and salinity gradients created with distance from flowing waters. The wet, low-salinity sediments in the center of the stream contained the most invertebrates and had the highest taxonomic diversity. Adjacent to the stream, communities in the hyporheic zone were influenced strongly by salt deposition. Abundance of invertebrates was low in the hyporheic zone, but this area contained the most co-occurring nematode species (three species). In dry soils, communities were composed almost entirely of a single species of nematode, Scottnema lindsayae, an organism not found in the stream center. These results suggest spatially-partitioned niches for invertebrates in soils and sediments in the dry valley landscape based on proximity to sources of moisture and the interactive effects of salinity. Received 22 September 1998; accepted 16 April 1999.     

Notes on some tardigrades from Thailand,with descriptions of two new species

Abstract

Three species of tardigrades are reported from Thailand: Pseudechiniscus quadrilobatus Iharos, 1969, Calcarobiotus (Calcarobiotus) digeronimoi sp. n., and Mixibius sutirae sp. n. Calcarobiotus (C.) digeronimoi sp. n. has claws of Calcarobiotus type; those of the first three pairs of legs have a medial and a lateral spur, those of the hind legs lack basal spurs. Mixibius sutirae sp. n. has a densely sculptured dorsal cuticle and two macroplacoids; it lacks lunules and other thickenings on the legs. It is similar to Mixibius ornatus Pilato et al., 2001, from which it differs in characteristics of the cu‐ticular sculpture and by having the ventral surface unsculptured.     

Tardigrade Distribution in a Medium-sized City of Central Argentina

The distribution and abundance of tardigrades in the city of General Pico (Argentina) are analyzed from samples collected during autumn and spring 2001. Sample sites included paved urban locations with different traffic intensities, non-paved periurban places, and places with peculiar conditions such as the city industrial area and the bus station. Trees of the same species were selected in each area and from each of them nine subsamples of lichens and/or moss, 11 mm in diameter, were taken with steel corers. The diversity, density and relative abundance of tardigrades was recorded and analyzed. Sampling sites were ordinated and classified with PCA and clustering. The number total of species collected in the research was 5. The maximum number of species per site and per tree was 4. The species recorded were: Echiniscus rufoviridis, Milnesium cf. tardigradum, Ramazzottius oberhaeuseri, Macrobiotus areolatus and an undescribed species of the genus Macrobiotus. The average density was approximately 10 specimens per cm² and the maximum values reach over 50 specimens per cm². R. oberhaeuseri and M. cf. tardigradum were the most frequent species. R. oberhaeuseri dominates in periurban areas with high suspension dust and very exposed to the sun. M. cf. tardigradum dominates on paved streets with intense vehicle traffic. Results supported the hypothesis of the relationship between air quality and tardigrade diversity.     

Variation in anhydrobiotic survival of two eutardigrade morphospecies: a story of cryptic species and their dispersal

Studies of geographic variation in anhydrobiotic tolerance may increase our understanding of the population dynamics of terrestrial meiofauna and the relative importance of local adaptation and microhabitat niche separation. Although anhydrobiosis in tardigrades has been studied extensively, few studies have dealt with intraspecific variation in survival and none of these included genetic data to validate the intraspecific nature of the comparisons. Such data are necessary when working with meiofauna as cryptic species are common. We analysed the anhydrobiotic survival and genetic variation in cytochrome oxidase subunit I of two eutardigrades ( Richtersius coronifer and Ramazzottius oberhaeuseri ) from Italy and Sweden to detect possible local adaptation. Survival was analysed as a multidimensional contingency table and showed that anhydrobiotic survival was higher in Sweden for Ra . oberhaeuseri whereas no significant geographic variation was found for Ri. coronifer . Our genetic analysis indicated the coexistence of two cryptic species of Ra . oberhaeuseri in Italy, only one of which was found in Sweden. It could not be determined whether the variation in Ramazzottius is intra- or interspecific due to the presence of these cryptic species. We suggest that geographic variation in anhydrobiotic survival may be a general phenomenon in tardigrades but further research is necessary to determine the degree of intraspecific variation. The genetic analysis showed indications of long-term isolation of the individual populations of Ri. coronifer but recent dispersal in one of the cryptic species of Ramazzottius . We found higher survival in Ra . oberhaeuseri than in Ri. coronifer . These results indicate a possible coupling between anhydrobiotic survival and dispersal rate.