Macromolecular composition of Palaeozoic scolecodonts: insights into the molecular taphonomy of zoomorphs

Dutta, S., Hartkopf‐Fröder, C., Mann, U., Wilkes, H., Brocke, R. & Bertram, N. 2010: Macromolecular composition of Palaeozoic scolecodonts: insights into the molecular taphonomy of zoomorphs. Lethaia, Vol. 43, pp. 334–343. Biogeochemistry and molecular taphonomy of biopolymers of marine zoomorphs are poorly known. In order to obtain insights into this issue we report on the biogeomacromolecular composition of hand‐picked, well‐preserved scolecodonts of Ordovician, Silurian and Devonian age using micro‐Fourier transform infrared (micro‐FTIR) spectroscopy, Curie point pyrolysis‐gas chromatography‐mass spectrometry (Cupy‐GC‐MS) and tetramethylammonium hydroxide (TMAH)‐assisted thermochemolysis‐GC‐MS. The present study reveals that scolecodonts are composed of both aliphatic and aromatic moieties. The micro‐FTIR spectra of scolecodonts are characterized by aliphatic CH_x (3000–2800 and 1460–1450/cm) and CH₃ (1375/cm) absorptions and aromatic C=C (1560–1610/cm) and CH (3050/cm and 700–900/cm) absorptions. The major pyrolysis products from the scolecodonts include aromatic hydrocarbons such as alkylbenzenes, alkylnaphthalenes and alkylphenols. Aliphatic hydrocarbons are represented by a homologous series of n‐alkenes and n‐alkanes. The compounds released upon thermochemolysis with TMAH are saturated and unsaturated fatty acids (as their methyl esters), n‐alkenes/alkanes and aromatic acids (as their methyl esters). No protein/amino acid‐derived compounds have been recognized in the pyrolysates or in the thermochemolysates, and it is concluded that protein/amino acid‐related compounds, which are commonly found in the jaws of extant polychaetes, were destroyed due to diagenetic processes. Obviously, excellent morphological preservation and low thermal alteration are not paralleled by a similar degree of chemical preservation. □Biogeomacromolecules, micro‐FTIR, pyrolysis‐GC‐MS, scolecodonts, thermochemolysis‐GC‐MS.     

Patterns and gradients of diversity in South Patagonian ombrotrophic peat bogs

Many north‐hemispherical mires seemingly untouched by drainage and cultivation are influenced by a diffuse sum of man‐made environmental changes, such as atmospherical nitrogen deposition that mask general patterns in species richness and functional group responses along resource gradients. To obtain insights into natural diversity‐environment relationships, we studied the vegetation and the peat chemistry of pristine bog ecosystems in southern Patagonia along a west–east transect across the Andes. The studied bog ecosystems covered a floristic gradient from hyperoceanic blanket bogs dominated by cushion building vascular plants via a transitional mixed type to Sphagnum‐dominated raised bogs east of the mountain range. To test the influence of resource availability on diversity patterns, species richness and functional groups were related to environmental variables by calculating general regression models and generalized additive models. Species richness showed strong linear correlations to peat chemical features and the general regression model resulted in three major environmental variables (water level, total nitrogen, NH₄Cl soluble calcium), altogether explaining 76% of variance. Functional group response illustrated a clear separation along environmental gradients. Mosses dominated at the low end of a nitrogen gradient, whereas cushion plants had their optimum at intermediate levels, and graminoids dominated at high nitrogen contents. Further shifts were related to NH₄Cl soluble calcium and water level. The models documented partly non‐linear relationships between functional group response and trophical peat properties. Within the three bog types, the calculated models differed remarkably illustrating the scale‐dependency of the explanatory factors. Our findings confirmed several general patterns of species richness and functional shifts along resource gradients in a surprisingly clear way and underpin the significance of undisturbed peatlands as reference systems for testing of ecological theory and for conservation and ecological restoration in landscapes with strong human impact.     

Behavioral and Physiological Thermoregulation of Crocodilians

Crocodilians, like other reptiles, regulate their body temperaturesby a combination of behavioral and physiological mechanisms.Behaviorally, they seek warm surface water or bask when cooland avoid overheating by the evaporation of water from theirdorsum, evaporation of water by gaping or by retreating to deep,cool water. Physiologically, crocodilians increase cutaneousthermal conductance by increasing blood flow to the skin (andsubdermal musculature) during warming. This hastens the warmingprocess. Cutaneous blood flow is reduced during general coolingand locally if the body temperature exceeds skin temperature.This enables crocodilians to increase body temperature significantlywhile basking in cool shallow water. Large crocodilians appearto be able to alter their rates of heat exchange to a largerextent than small ones and they can do so with less cardiovascularinvolvement. Large crocodilians, with their lower surface/volumeratio, are capable of producing sufficient metabolic heat toelevate their body temperature above water temperature.     

Vegetational patterns and distribution of relict taxa in humid temperate forests and wetlands of Georgia (Transcaucasia)

Small-scale vegetational patterns of Georgian lowland and montane forests and wetlands are documented by species per vegetation unit, function of species in particular vegetation units and vegetational sketches. The humid warm-temperate climate of western Georgia contributes to a different spatial pattern than known for most of Europe. One characteristic feature of western Georgian relict vegetation is the co-occurrence of 'Mediterranean', 'Sub-mediterranean', temperate, and Tertiary relict species, as well as of species normally confined to either zonal or azonal vegetation, in the same or closely related vegetation units. The extant distribution of Tertiary relict taxa strongly depends on how they are niching into changing environments. Niching strategies are assumed crucial for extinction or survival in times of rapid climatic/environmental changes. For Tertiary relict plant taxa in western Georgia we found four different niching strategies which also hold true of other northern hemispheric Tertiary relict plant taxa. Some amphibians and reptiles display similar distribution patterns and niching strategies as do relict plant taxa. A number of relict taxa in the warm humid regions of western Georgia occupy niches in swamp forests which might represent 'primeval' environments of species which are at present also elements of meso-Mediterranean vegetation and of thermophilous forest edges and hedges in Central Europe.     

Ultimate Fate of Rod Outer Segments in the Retinal Pigment Epithelium

To investigate the degradation pathway of rod outer segments (ROS) in vivo, we injected gold-labeled ROS into the subretinal space of rabbits using a pars plana approach. Histology and electron microscopy performed on the specimens 72 hr after ROS injection revealed that the retina over the injection site was reattached, the retinal pigment epithelial (RPE) cells were intact, and gold granules were localized inside melanin granules and melanosomes. These results indicate that, in RPE, in vivo degradation of ROS is associated with melanosomes.     

Isotypes in Human Immunoglobulin λ-Chains

IMMUNOGLOBULIN polypeptide chains consist of a variable N-terminal region and a constant C-terminal part¹. The variability of the N-terminal part is due to multiple amino-acid exchanges and deletions, which can be arranged into chemically distinct subgroups^2–9. The C-terminal part is characterized by single amino-acid substitutions in an otherwise constant, yet chain type specific, sequence^1,10–12.