Empirical evidence of alternative stable states in an estuary.

Due to human activity, ecosystems are exceeding their ecological thresholds and shifting into undesired alternative stable states with new ecological configurations. Despite their purported ubiquity, it is uncertain whether estuaries can exist in multiple stable states. We use data from a 3.5-year study of invertebrate communities in an Australian estuary that is usually closed to the ocean to test for their existence. Sampling spanned a 1.5-year period of hypersalinity (>40 ppt) during a prolonged estuary closure, where salinity reached 122 ppt, and for two years during and after the estuary opened to the ocean when salinities were mesohaline (5-19 ppt). Two distinct community states occurred before and after the sandbar breached, with an intermediary period of invertebrate community impoverishment due to sediment scouring. During the closure, the community was simple (average of one taxa 100 cm-2) and dominated by larvae of terrestrial insects, most notably the halotolerant, non-biting midge Tanytarsus barbitarsis. After opening, the richness and abundance of invertebrates increased (average of four taxa and 84 individuals 100 cm-2) as polychaetes, molluscs and crustaceans colonised the estuary, although recovery was incomplete according to previous species records. Duration of estuary closure and salinity were the strongest drivers of composition. This study, together with evidence from the literature, suggests a salinity threshold of 60-65 ppt between states. These empirical data meet key criteria of alternative states, i.e. a clear transition between two distinct self-sustaining communities, indicating a regime shift triggered by an exogenous event. Our findings suggest that temporarily open and closed estuaries can exist in alternative stable states, with prolonged closures, hypersalinity, and sandbar breaching being key determinants of the switch between states. This situation may apply to other low-inflow estuarine systems, particularly in arid, semi-arid, or seasonally arid climates, and may become more frequent with human-induced climate change.

Phylogeny of the genus Aleochara inferred from mitochondrial cytochrome oxidase sequences (Coleoptera: Staphylinidae).

The phylogeny of the genus Aleochara was previously poorly understood due to difficulties with phylogenetic reconstruction by morphological characters. We present here a phylogeny based on the sequences of a 2022-bp fragment of the COI/II genes; 50 Aleochara and 10 outgroup species were included in the analysis. We used parsimony, minimum-evolution, and maximum-likelihood analyses to infer the phylogeny of the group. Our data do not support the commonly assumed sister group relationship between Aleocharini and Hoplandriini. Aleochara is resolved as a monophylum, although A. clavicornis might not belong to the genus. Within Aleochara, there are two large monophyletic clades. Many of the existing subgenera are shown to be para- or polyphyletic; others are likely to be monophyletic. Tinotus morion, previously assigned to the Hoplandriini, is strongly supported as belonging to Aleochara. According to our data, the mesosternal carina that has been used as an important character for classification has arisen and been reduced independently in several clades within Aleochara.

Polyelectrolyte counterion condensation theory explains differential scanning calorimetry studies of salt-induced condensation of chicken erythrocyte chromatin.

The salt-induced chromatin condensation in chicken erythrocyte nuclei is studied by differential scanning calorimetry (DSC). The degree of chromatin condensation is measured for condensation induced by monovalent, divalent, trivalent, or tetravalent cations and by a mixture of sodium and magnesium. These last two cations show an evident competition effect. Salt-induced chromatin condensation is shown to be an entropy-driven process. A simple model of chromatin based on the polyelectrolyte counterion condensation theory is used in order to compute the charge neutralized by the cations in each chromatin domain. The degree of chromatin condensation is shown to be related to the weighed sum of the square of the phosphate charge of each domain. The model predicts the salt and the chromatin concentration dependence of the condensation and the effect of H1 removal.

Cardiovascular reactions and respiratory events during platelet activating factor-induced shock.

The platelet activating factor (PAF), a low molecular phospholipid, plays an important role in inflammation, anaphylaxis, and shock state development. In the isolated perfused guinea pig heart, PAF induces a decrease in coronary flow and cardiac contractility and atrioventricular conduction disturbances. Furthermore, PAF mediates a powerful bronchoconstrictory action causing a severe impairment in respiratory function. In the present study an attempt was made to separate cardiac from respiratory events during PAF-induced shock in vivo. PAF was injected intravenously (0.1-10 micrograms/kg) into anesthetized guinea pigs ventilated with room air or 100% oxygen. Administration of 10 micrograms/kg PAF was uniformly lethal: already within 2 min, cardiac output decreased by 60% and end-diastolic left ventricular pressure increased markedly indicating cardiac failure. ECG recordings showed signs of acute myocardial ischemia. Arrhythmias occurred in terms of atrioventricular conduction delay. Blood pressure initially increased, then declined continuously to below baseline within 10 min. All animals died within 25 min. Ventilation with room air was paralleled by development of severe hypoxia. However, under ventilation with 100% oxygen a dissociation between PAF-mediated cardiac and respiratory effects occurred. It is concluded that the PAF-induced shock is primarily based on direct cardiac damage. Furthermore, the ECG signs of ischemia are most likely due to coronary spasms.