Predicted suitable <i>Chimarrogale himalayica</i> habitat based on current (a) and (b) historical climatic conditions.

<p>The colors indicate the probability of a habitat being suitable. White indicates areas without climate data. Red dashed lines indicate boundaries for the distributions of the three subspecies of <i>Chimarrogale himalayica</i>. Gray circles indicate the localities used to construct the model. White triangles indicate distribution localities summarized by Corbet and Hill [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0077156#B3" target="_blank">3</a>].</p

Bayesian phylogenetic results, with divergence time estimations.

<p>This is a fossil-calibrated chronogram of a Bayesian phylogenetic analysis, which was constructed from mitochondrial DNA cytochrome <i>b</i> sequences, with a relaxed molecular clock. Branch length indicates the time of divergence. Node bars indicate the 95% credible interval for node ages. Numbers above branches indicate the posterior probabilities supporting each node. Letters below the branch nodes indicate the node numbers correlated with <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0077156#pone-0077156-t004" target="_blank">Table 4</a>. The four main clades are shaded with different colors (clades A to D). Red stars indicate fossil-calibrated nodes. The green star indicates the calibration for <i>Chimarrogale</i> living in China. Correlated Epochs and ages are shown. Current and recommended taxonomic statuses are also shown.</p

Hypothetical biogeographic history of Asiatic water shrews.

<p>Ancestral distribution of Asiatic water shrews (in shaded gray color) during the late Miocene in East and Southeast Asia (a). The population decreased during warming in the early Pliocene (b). The population expanded and re-colonized surrounding areas during the glaciation that occurred at the Pliocene/Pleistocene boundary (c). The population decreased again during warming in the early Pleistocene. The colors indicate corresponding geographical regions shown in <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0077156#pone-0077156-g004" target="_blank">Figure 4</a>. The distribution range of <i>Chimarrogale styani</i> is shown in pink (d). Population increases and decreases are indicated by arrows. Roman numerals indicate the three possible refuges. Question marks indicate an unknown refuge area in East Asia. The ranges of the southwestern Tibetan Plateau are shown in bold red lines. </p

Pretest phylogenetic results for Asiatic water shrews.

<p>The results of an analysis of mitochondrial DNA cytochrome <i>b</i> sequences via the maximum likelihood method with 1,000 bootstrap replicates are shown. (a) Consensus tree and (b) 50% condensed tree. Numbers on nodes indicate bootstrap support values.</p

Operando Measurement of Solid Electrolyte Interphase Formation at Working Electrode of Li-Ion Battery by Time-Slicing Neutron Reflectometry

We report the first operando measurement of solid electrolyte interphase (SEI) formation at an electrode using in situ neutron reflectometry. The results revealed the growth of the SEI and intercalation of ions during the charge reaction. Furthermore, we propose a way of evaluating the charge used for the SEI formation

Проект кафе "Новое время" на 54 места

Текст работы публикуется с изъятиям

Additional file 1: Table S1. of Morphological and molecular characteristics of Malayfilaria sofiani Uni, Mat Udin & Takaoka n. g., n. sp. (Nematoda: Filarioidea) from the common treeshrew Tupaia glis Diard & Duvaucel (Mammalia: Scandentia) in Peninsular Malaysia

Comparison of measurements of Malayfilaria sofiani n. g., n. sp. from common treeshrews in Malaysia with other filarial species recorded from treeshrews or hosts in the same geographical region. (XLSX 18 kb