Effects of hydrological forcing on the structure of a tropical estuarine food web

River flow can impact which sources of particulate organic matter (POM) fuel estuarine food webs. Here, we used stable carbon (C) and nitrogen (N) isotope analyses to compare how contributions of different POM sources (terrestrial, estuarine, and marine) to the diets of zooplankton and juvenile fishes differed between low and high river flow conditions, as well as spatially across a tropical estuary, Hilo Bay, Hawaii, USA. Diets of zooplankton and juvenile fishes were affected by river flow conditions, but the magnitude and the change in the basal resources depended on the location of the station in the estuary relative to the ocean and the river mouths. Consumers from the station most isolated from the ocean and with groundwater and overland flow inputs, utilized a combination of estuarine and terrestrial POM during both low and high river flow conditions and exhibited less variability in their basal resources than stations with direct ocean exchange. Consumers from stations in the Bay most affected by ocean exchange and river inputs utilized a combination of estuarine, terrestrial, and marine POM during low flow conditions, but shifted to marine and terrestrial POM during high river flow conditions. This shift to using terrestrial POM during high river flow conditions was substantial and up to 40% higher than values measured in other estuaries. Factors suspected to be affecting which POM source(s) consumers use in Hilo Bay are gross primary production, biological availability of exported terrestrial OM, and estuarine bacteria biomass, all of which are affected by river flow. Overall, our results suggest that Hilo Bay's food web and possibly those from other tropical estuaries are vulnerable to changes in hydrology, which may be further enhanced by global climate change.     

Comparative multi-locus phylogeography confirms multiple vicariance events in co-distributed rainforest frogs

Though Pleistocene refugia are frequently cited as drivers of species diversification, comparisons of molecular divergence among sister species typically indicate a continuum of divergence times from the Late Miocene, rather than a clear pulse of speciation events at the Last Glacial Maximum. Community-scale inference methods that explicitly test for multiple vicariance events, and account for differences in ancestral effective population size and gene flow, are well suited for detecting heterogeneity of species' responses to past climate fluctuations. We apply this approach to multi-locus sequence data from five co-distributed frog species endemic to the Wet Tropics rainforests of northeast Australia. Our results demonstrate at least two episodes of vicariance owing to climate-driven forest contractions: one in the Early Pleistocene and the other considerably older. Understanding how repeated cycles of rainforest contraction and expansion differentially affected lineage divergence among co-distributed species provides a framework for identifying evolutionary processes that underlie population divergence and speciation.     

Association energetics of membrane spanning alpha-helices

Since Popot and Engelman proposed the 'two-stage' thermodynamic framework for dissecting the energetics of helical membrane protein folding, scientists have endeavored to measure the free energies of helix-helix associations to better understand how interactions between helices stabilize and specify native membrane protein folds. Chief among the biophysical tools used to probe these energies are sedimentation equilibrium analytical ultracentrifugation, fluorescence resonance energy transfer, and thiol disulfide interchange experiments. Direct and indirect comparisons of thermodynamic results suggest that differences in helix-helix stabilities between micelles and bilayers may not be as large as previously anticipated. Genetic approaches continue to become more quantitative, and the propensities for helices to interact in bacterial membranes generally correlate well with in vitro measurements.     

Pectenotoxin and okadaic acid-based toxin profiles in Dinophysis acuta and Dinophysis acuminata from New Zealand

The major pectenotoxin and okadaic acid group toxins in Dinophysis acuta and Dinophysis acuminata cell concentrates, collected from various locations around the coast of the South Island of New Zealand (NZ), were determined by liquid chromatography–tandem mass spectrometry (LC–MS/MS). PTX2 and PTX11 were the major polyether toxins in all Dinophysis spp. cell concentrates. D. acuta contained PTX11 and PTX2 at concentrations of 4.7–64.6 and 32.5–107.5 pg per cell, respectively. The amounts of PTX11 and PTX2 in D. acuminata were much lower at 0.4–2.1 and 2.4–25.8 pg per cell, respectively. PTX seco acids comprised only 4% of the total PTX content of both D. acuta and D. acuminata. D. acuta contained low levels of OA (0.8–2.7 pg per cell) but specimens from the South Island west coast also contained up to 10 times higher levels of OA esters (7.0–10.2 pg per cell). Esterified forms of OA were not observed in D. acuta specimens from the Marlborough Sounds. D. acuta did not contain any DTX1 though all D. acuminata specimens contained DTX1 at levels of 0.1–2.4 pg per cell. DTX2 was not present in any New Zealand Dinophysis spp. specimens. Although the total toxin content varied spatially and temporally, the relative proportions of the various toxins in different specimens from the same location appeared to be relatively stable. The total PTX/total OA ratios in different isolates of D. acuta were very similar (mean±S.E.: 14.9±1.9), although the Marlborough Sounds D. acuminata isolates had a higher total PTX/total OA ratio (mean±S.E.: 22.7±2.4) than the Akaroa Harbour isolates (8.0). No evidence of azaspiracids were detected in these specimens. These results show that the LC–MS/MS monitoring of plankton for PTX group toxins (e.g. PTX2) and their derivatives (e.g. PTX2 seco acid) may provide a sensitive, semi-quantitative, indicator of the presence of more cryptic OA group toxins (e.g. OA esters).     

Evidence for numerous analogs of yessotoxin in Protoceratium reticulatum

A solid-phase extract from Protoceratium reticulatum was partitioned between water and butanol and the two fractions purified on an alumina column. Fractionation was monitored by ELISA and LC–MS. Results indicate that while almost all yessotoxin (1) was extracted into butanol, large amounts of yessotoxin analogs remained in the aqueous extract along with lesser amounts in the butanolic extract. NMR analysis of selected fractions from reverse-phase chromatography of the extracts confirmed the presence of yessotoxin analogs, although structure determinations were not possible due to the complexity of the mixtures. Analysis of fractions with LC–MS³ and neutral-loss LC–MS/MS indicated the presence of more than 90 yessotoxin analogs, although structures for most of these have not yet been determined. These analogs provide a mechanism to rationalise the discrepancy between ELISA and LC–MS analyses of algae and shellfish.