Ferri- and Ferrocyanide Salts Change the Current/Voltage Relations of Chara corallina: No Correlation with the Transmembrane Redox System

The current/voltage {I/V) relations of the plasma membrane ofChara corallina cells are characteristic when the bathing mediumhas elevated (5-0 mM) concentrations of potassium Addition ofeither 0-5 mM femcyanide or 0-5 mM ferrocyanide usually induceda qualitatively similar increase in the ‘leak’ current,with a concomitant increase in membrane conductance. Both redoxreactants failed for unknown reasons to affect the I/V profileof some of the cells tested In the sensitive cells, femcyanidewas unable to generate extra current over that found upon additionof ferrocyanide Because the feiTocyanide oxidation rate of thecells is only 10% of the femcyanide reduction rate, we concludethat both forms, fern- and ferrocyanide, affect the 'leak' conductanceindependent of the redox state of the reactants, i e ferrocyanidedoes not act indirectly via an oxidation to femcyanide Hence,under the experimental conditions, we were unable to detecta current that could be assigned to the operation of a transmembraneredox system Furthermore, the fern- and ferrocyanide inducedshift in the I/V profile only reversed slowly after withdrawalof the redox reactants. This suggests that the elicited currentis independent of the presence of an extracellular electronacceptor, i.e on the continuous operation of a proposed transmembraneredox system Key words: Current/voltage curves, transmembrane reductase, voltage clamp, femcyanide, ferrocyanide, Chara     

Miocene methane‐derived carbonates from southwestern Washington,USA and a model for silicification at seeps

Kuechler, R.R., Birgel, D, Kiel, S, Freiwald, A, Goedert, J.L., Thiel, V & Peckmann, J. 2011: Miocene methane‐derived carbonates from southwestern Washington, USA and a model for silicification at seeps. Lethaia, Vol. 45, pp. 259–273. Exotic limestone masses with silicified fossils, enclosed within deep‐water marine siliciclastic sediments of the Early to Middle Miocene Astoria Formation, are exposed along the north shore of the Columbia River in southwestern Washington, USA. Samples from four localities were studied to clarify the origin and diagenesis of these limestone deposits. The bioturbated and reworked limestones contain a faunal assemblage resembling that of modern and Cenozoic deep‐water methane‐seeps. Five phases make up the paragenetic sequence: (1) micrite and microspar; (2) fibrous, banded and botryoidal aragonite cement, partially replaced by silica or recrystallized to calcite; (3) yellow calcite; (4) quartz replacing carbonate phases and quartz cement; and (5) equant calcite spar and pseudospar. Layers of pyrite frequently separate different carbonate phases and generations, indicating periods of corrosion. Negative δ¹³C_carbonate values as low as ?37.6‰ V‐PDB reveal an uptake of methane‐derived carbon. In other cases, δ¹³C_carbonate values as high as 7.1‰ point to a residual, ¹³C‐enriched carbon pool affected by methanogenesis. Lipid biomarkers include ¹³C‐depleted, archaeal 2,6,10,15,19‐pentamethylicosane (PMI; δ¹³C: ?128‰), crocetane and phytane, as well as various iso‐ and anteiso‐carbon chains, most likely derived from sulphate‐reducing bacteria. The biomarker inventory proves that the majority of the carbonates formed as a consequence of sulphate‐dependent anaerobic oxidation of methane. Silicification of fossils and early diagenetic carbonate cements as well as the precipitation of quartz cement – also observed in other methane‐seep limestones enclosed in sediments with abundant diatoms or radiolarians – is a consequence of a preceding increase of alkalinity due to anaerobic oxidation of methane, inducing the dissolution of silica skeletons. Once anaerobic oxidation of methane has ceased, the pH drops again and silica phases can precipitate. □Biomarkers, carbonates, isotopes, methane, Miocene, silicification, Washington.     

An evolutionary fast‐track to biocalcification

The ability to construct mineralized shells, spicules, spines and skeletons is thought to be a key factor that fuelled the expansion of multicellular animal life during the early Cambrian. The genes and molecular mechanisms that control the process of biomineralization in disparate phyla are gradually being revealed, and it is broadly recognized that an insoluble matrix of proteins, carbohydrates and other organic molecules are required for the initiation, regulation and inhibition of crystal growth. Here, we show that Astrosclera willeyana, a living representative of the now largely extinct stromatoporid sponges (a polyphyletic grade of poriferan bauplan), has apparently bypassed the requirement to evolve many of these mineral‐regulating matrix proteins by using the degraded remains of bacteria to seed CaCO₃ crystal growth. Because stromatoporid sponges formed extensive reefs during the Paelozoic and Mesozoic eras (fulfilling the role that stony corals play in modern coral reefs), and fossil evidence suggests that the same process of bacterial skeleton formation occurred in these stromatoporid ancestors, we infer that some ancient reef ecosystems might have been founded on this microbial–metazoan relationship.     

Effects of Recreation and Hunting on Flushing Distance of Capercaillie

Abstract: The capercaillie (Tetrao urogallus) in Central Europe is an endangered species of grouse that is thought to be highly susceptible to human disturbance, possibly causing local populations to decline. We investigated the behavioral response of capercaillie in the Black Forest, Germany, and the French Pyrenees to an off-trail hiker by measuring flushing distances. Flushing distance varied with capercaillie sex, visibility of the hiker, intensity of winter tourism, and hunting pressure. Independent of the study area, males flushed at consistently longer distances than females, and lower visual blocking between bird and hiker resulted in longer flushing distances. Capercaillie flew at longer distances from an approaching hiker in areas with high intensity of winter tourism or hunting pressure than in undisturbed areas. We recommend the establishment of regulations requiring hikers to stay on trails and to close trails where intertrail distances fall below 100 m (90% of all flushing events appeared within 50 m). Furthermore, planting or preserving evergreen conifer trees in dense rows along critical parts of disturbance sources, reducing the degree of visibility between capercaillie and recreationists would increase habitat for capercaillie in forests with predictable recreation activities.