Pro‐inflammation and pro‐fibrosis factors were highly induction in heart tissues of carotid arteries balloon‐injured animal model

To investigate the changes of cardiomyocyte inflammation and fibrosis factors in heart of carotid artery balloon injury inflammatory rat model. Using rat carotid artery balloon injury model to detect left ventricular characteristics at 2 h, 2 days and 14 days after surgery using hematoxylin‐eosin (H&E) gross stain, Masson's trichome stain and Western blot analysis for inflammatory and fibrosis‐induced factors, tumour necrosis factor α (TNFα), JNK1, P38α, connective tissue growth factor (CTGF), SP1 and transforming growth factor β (TGFβ) protein expressions. The rat carotid arteries were injured after 2 h, 2 days and 14 days. Balloon‐angioplasty to H&E stain results showed the increasing trend of left ventricular wall at 2 h and 2 days; then, the left ventricular wall became thinner, and the left ventricular chamber became enlarged and dilated after 14 days of carotid artery balloon injury. In addition, the Masson's trichome stain results showed that the left ventricular section has fibrosis‐related blue staining (collagen) at 2 and 14 days after rat carotid artery balloon injury, and became even more severe at 14 days. Furthermore, we observed the protein expression level changs, which include TNFα, JNK1, P38α, CTGF, SP1 and TGFβ using Western blotting assay. All proteins were induced at 2 h, 2 days and then reached the maximal level at 14 days. The vessel inflammation was associated with cardiac inflammatory and fibrosis effects during or after carotid artery balloon injury. Copyright © 2012 John Wiley & Sons, Ltd.     

Particle selectivity of pelagic tintinnid agglutination

Scanning electron microscopic observation reveals that several agglutinated, pelagic tintinnid taxa apparently possess a capability of incorporating specific mineral grains, such as monospecific coccoliths, for their loricae. Since the ocean water generally contains other coccolith taxa, as well as diatoms and clays, it seems possible that the tintinnids can single out a particular coccolithophore species from the variety of suspended matter for their loricae-building.     

Molecular and morphological evidences reveal a cryptic species in the Vinaceous Rosefinch Carpodacus vinaceus (Fringillidae; Aves)

Wu, H.‐C., Lin, R.‐C., Hung, H.‐Y., Yeh, C.‐F., Chu, J.‐H., Yang, X.‐J., Yao, C.‐J., Zou, F.‐S., Yao, C.‐T., Li, S.‐H. & Lei, F.‐M. (2011). Molecular and morphological evidences reveal a cryptic species in the Vinaceous Rosefinch Carpodacus vinaceus (Fringillidae; Aves). —Zoologica Scripta, 40, 468–478. The Vinaceous Rosefinch (Carpodacus vinaceus) is endemic in East Asia with two recognized subspecies –C. v. vinaceus, distributed along the eastern edge of the Tibetan Plateau and the Himalayas, and C. v. formosanus, restricted to Taiwan’s Central Mountain Range. As reflected in a controversial taxonomic history, this vastly disjunctive distribution pattern suggests that the subspecies, having been isolated from each other for a long time, might have diverged, challenging the current taxonomic treatment and calling for possible species delimitation. Sequences of two mitochondrial fragments (mtDNA) and two Z‐linked nuclear loci (zDNA) were used to reconstruct the intraspecific phylogeny of C. vinaceous. The mtDNA tree shows that the two subspecies of the vinaceous rosefinch form two exclusively monophyletic clades. All but one zDNA sequences from the nominate subspecies and C. v. formosanus also formed exclusively monophyletic clades (the exceptional zDNA sequence from C. v. vinaceous formed a weakly supported clade with two outgroup species). Moreover, by conducting quantitative comparisons of morphometric traits and male plumage coloration, we found that the two subspecies exhibit distinguishable morphological differences. All the evidence therefore suggests that C. v. formosanus is a cryptic species and that its taxonomic status should be restored to full species. Molecular dating suggests that the two sibling rosefinches split 1.7 ± 0.2 million years ago, providing a point estimate for the historical connectivity of biota between eastern Tibet‐Himalayas and montane Taiwan.