Euryhalinity of Palaeozoic articulate brachiopods

OMonotypic and very low diversity virgianid shell beds from the Upper Ordovician to Lower Silurian dolomites of North Greenland were formed in marginal marine quiet-water hypersaline environments. In the light of this evidence the salinity tolerances of other Palaeozoic articulate brachiopods is evaluated. There are only a small number of species apparently invading hypersaline or brackish environments, but it is significant considering that previously all articulate brachiopods were thought to be fully marine. Two types of occurrence are noted, those species specifically related to marginally marine environments, disappearing with the introduction of fully marine faunas, and the majority of species which extend their normal marine range into marginal conditions. No brachiopod species appears to have invaded very hypersaline or truly brackish conditions. No single group of articulate brachiopods specifically specialised in colonising marginal marine environments, apart from possibly the virgianid pentamerids. Palaeozoic, Upper Ordovician, Lower Silurian, Brachiopoda. Pentamerida, Virgianidae, Greenland, palaeoecology. hypersaline environments, brackish environments .     

PARTIAL CHARACTERIZATION OF A PUTATIVE 110kDa MYOSIN FROM THE GREEN ALGACHARA CORALLINABYIN VITROBINDING OF FLUORESCENT F-ACTIN

Using the binding of heterologous, rhodamine phalloidin-labelled F-actinin vitro, two F-actin binding proteins were identified in protein extracts from the green algaChara corallinaafter fractionation by anion exchange chromatography. The first protein, a putative myosin, released laterally bound F-actin at ATP-concentrations as low as 1μm ; equivalent concentrations of ADP were not effective. Binding of F-actin was inhibited by the sulfhydryl-alkylating agent N-ethylmaleimide (NEM). Binding of F-actin was also abolished by a monoclonal anti-myosin (J14) previously used for immunodetection and immunolocalization in internodal cells (Groliget al., 1988,Eur J Cell Biol 47 : 22–31). Immunoblotting with J14 detected a 110kDa polypeptide only in those protein fractions that had revealed ATP-sensitive binding of F-actin. The putative myosin bound with mediocre affinity to immobilized calmodulin and free Ca²⁺-concentration made no difference to this binding affinity. In contrast to the putative myosin, the second, less abundant protein revealed ATP-insensitive and end-wise binding to the microfilament and was not recognized by the anti-myosin antibody.     

Behavioural interpretation of a rosetted spreite trace fossil: Dactyloidites ottoi (Geinitz)

Excellently preserved specimens of the trace fossil Haenrzschelinia onoi (Geinitz) allow its three-dimensional reconstruction and interpretation of the behaviour underlying the morphological pattern. H. onoi is a rosette-shaped endogenic trace fossil comprising central tube and branching incomplete radial protrusive spreiten. The basic behaviour pattern (rosetted vertical spreiten with central shaft) is the same as that of Brooksella Walcott 1896 and Dactyloidites Hall 1886. Haentzschelinia is therefore placed in synonymy with Dactyloidites , which has priority.     

Storage and turnover of carbon in grassland soils along an elevation gradient in the Swiss Alps

Amount, composition, and rate of turnover of soil organic carbon (SOC) in mountainous cold regions is largely unknown, making predictions of future responses of this carbon (C) to changing environmental conditions uncertain. We hypothesized increasing amounts and declining turnover times of soil organic matter (SOM) under permanent grassland with increasing elevation and decreasing temperature. Samples from an irrigated transect in the Swiss Alps (880 to 2200 m elevation, mean annual temperatures +8.9 to +0.9 °C) were analyzed. Soil C stocks ranged from 49 to 96 t C ha⁻¹ (0–20 cm) and were not related to elevation, though the highest site stored least C. Particulate organic carbon (POC) increased significantly with elevation and accounted for > 80% of the total soil C at 2200 m (0–5 cm). Mean residence times (MRTs) of POC computed by means of radiocarbon dating were in the order of years to decades and were positively related to elevation in the topsoil. At higher elevations, the estimated total C flux through the soil profile mainly depended on this fraction. MRT of mineral-associated matter ranged from decades to centuries and was not systematically related to elevation, but positively related to the soil mineral surface area and it increased with soil depth. Turnover rates from simulations with the soil C model RothC exceeded those from ¹⁴C measurements by a factor of 1.7–3.3 which suggests that C dynamics at these sites is overestimated by the model. Size of model pools and amount of C in soil fractions were only weakly correlated, thereby challenging previously postulated hypotheses concerning the correspondence of pools and fractions for grasslands at higher elevations.     

The influence of faunal condensation and mixing on the preservation of fossil benthic communities

Fürsich. Franz Theodor 1978 07 IS: The influence of faunal condensation and mixing on the preservation of fossil benthic communities. Lethaia , Vol. 11, pp. 243–250. Oslo. ISSN 0024–1164.
Condensation phenomena caused by environmental, biotic, or diagenetic factors are widespread in the fossil record, especially in shallow shelf sediments, and may alter the composition of ancient communities. Even without large-scale transport being involved, often only time-averaged seres will be available for palaeosynecological studies. This should be kept in mind when community analysis of such shell accumulations is attempted.