影像分析在生化研究中的应用概况

影像分析是一项重要的微观物质形态测量和浓度测量技术,已经在众多领域中得到应用。本主要介绍影像分析系统的基本结构及其在生化领域中的应用情况,包括细胞形态观察与测量、突变菌株的区分与筛选、蛋白质与ＤＮＡ分子浓度的测量。     

The phylogeny of charadriiform birds (shorebirds and allies) – reassessing the conflict between morphology and molecules

Multiple molecular analyses provide a congruent and well‐supported phylogeny of the charadriiform family‐level taxa, which conflicts with previous hypotheses based on osteological data. In order to revise the latter and to identify new characters of phylogenetic significance, skeletons of most charadriiform family‐level taxa were examined and 49 characters analysed. Tree topology was sensitive to outgroup choice, but the result of the analysis rooted with Columbidae (doves and pigeons) recovered a monophyletic Scolopaci, Charadrii, and nonturnicid Lari. With regard to the inclusion of Alcidae and Glareolidae in the Lari, the results of the present study are also in better concordance with the new molecular phylogenies than previous analyses of morphological data. Furthermore, for the first time an apomorphy of a clade including Thinocoridae, Pedionomidae, Rostratulidae, and Jacanidae was identified. Inclusion of Turnicidae in the Lari could not be supported, but there is no strong morphological evidence for an alternative placement. Pluvianus shares derived osteological features with the Burhinidae, and its position in the molecular analyses likewise cannot be corroborated with morphological data. Based on the topology of the molecular consensus tree, the ancestral state of selected characters is reconstructed. It is finally noted that recent calibrations of molecular analyses, which indicate an origin of extant charadriiform lineages in the Cretaceous, are based on incorrectly identified fossils. © 2011 The Linnean Society of London, Zoological Journal of the Linnean Society, 2011, 161 , 916–934.     

Island evolutionary biogeography: analysis of the weevils (Coleoptera: Curculionidae) of the Falkland Islands (Islas Malvinas)

Aim I analysed distributional and phylogenetic information on weevils (Coleoptera: Curculionidae) from the Falklands, and integrated it with molecular, palaeontological and geological information to infer a geobiotic scenario. Location Falkland Islands (Islas Malvinas). Methods The panbiogeographical analysis was based on data on 23 Falkland species and their related taxa from southern South America. For the cladistic biogeographical analysis I analysed six weevil taxa for which phylogenetic hypotheses are available (the generic groups Cylydrorhinus, Strangaliodes and Falklandius, and the genera Antarctobius, Germainiellus and Puranius). Results from this analysis were compared with previous regionalizations. Cenocrons (sets of taxa that share the same biogeographical history) were identified by considering temporal information provided by fossils and molecular clocks. Finally, a geobiotic scenario was proposed by integrating the available information. Results Six generalized tracks were detected: Maule–Valdivian forests, Magellanic forest, Magellanic moorland, Falkland Islands, Magellanic forest–Magellanic moorland, and Magellanic forest–Falkland Islands. A node was identified in the Magellanic forest, based on the overlap of two generalized tracks. A single general area cladogram was obtained, implying the following sequence: (Magellanic moorland (Maule–Valdivian forests (Magellanic forest, Falkland Islands))). The Falklands are classified here as a biogeographical province in the Austral realm, Andean region and Subantarctic subregion. Falkland weevils seem to belong to a single Subantarctic cenocron. The sequence of events deduced implies the following steps: development of the Subantarctic biota in southern South America, arrival of the Falkland crustal block from South Africa in the Early Cretaceous, geodispersal of the Subantarctic cenocron from southern South America to the Falklands during the Early Oligocene, vicariance of the Magellanic moorland, vicariance of the Maule–Valdivian forests, and final vicariance between the Magellanic forest and the Falkland Islands. Main conclusions The biotic components identified support the connection of the Falkland weevils with the Magellanic forest. Falkland weevils belong to a single cenocron, dated to at least the Early Oligocene, when geodispersal from southern South America may have occurred. An older African cenocron may have been replaced completely by the Subantarctic one when the proto‐Falklands made contact with the Patagonian continental shelf. A geobiotic scenario implying vicariance events related to sea‐level variations could explain the distributional patterns analysed herein.     

Fungal catabolic gene regulation: Molecular genetic analysis of theamdS gene ofAspergillus nidulans

Aspergillus nidulans is an excellent experimental organism for the study of gene regulation. Genetic and molecular analyses oftrans-acting andcis-acting mutations have revealed a complex pattern of regulation involving multiple independent controls. Expression of theamdS gene is regulated by thefacB andamdA genes which encode positively acting regulatory proteins mediating a major and a minor form of acetate induction respectively. The product of theamdR gene mediates omega amino acid induction ofamdS. The binding sites for each of these proteins have been localised throughamdS cis-acting mutations which specifically affect the interaction with the regulatory protein. The global controls of nitrogen metabolite repression and carbon catabolite repression regulate the expression of many catabolic genes, includingamdS. Nitrogen control is exerted through the positively actingareA gene product and carbon control is dependent on thecreA gene product. Each of the characterized regulatory genes encodes a DNA-binding protein which recognises particular sequences in theamdS promoter to activate or repress gene expression. In addition, there is evidence for other genetically uncharacterised proteins, including a CCAAT-binding complex, which interact with the 5 region of theamdS gene.     

Faunal changes and geographic crypticism indicate the occurrence of a biogeographic transition zone along the southern East Pacific Rise

Aim Deep‐sea hydrothermal vents have now been reported along all active mid‐ocean ridges and back‐arc basins, but the boundaries of biogeographic entities remain questionable owing to methodological issues. Here we examine biogeographic patterns of the vent fauna along the East Pacific Rise (EPR) and determine the relative roles of regional and local factors on the distribution of biodiversity associated with mussel beds along a poorly explored zone, the southern EPR (SEPR). Location East Pacific Rise. Methods A species list of macrobenthic invertebrates along the EPR was compiled from the literature and supplemented with data recovered during the French research cruise BIOSPEEDO carried out in 2004 along the SEPR. Biogeographic patterns were assessed by combining the identification of morphological species with a molecular barcoding approach. A multivariate regression tree (MRT) analysis was performed to identify any geographic breaks, and an empirical distribution of species richness was compared with predictions provided by a mid‐domain effect model. Macrofaunal community structure associated with mussel beds along the SEPR was analysed in relation to environmental factors using cluster and canonical redundancy analyses. Results Sequencing of the cytochrome c oxidase subunit I gene revealed the occurrence of several cryptic species complexes along the EPR, with the equator separating the southern and northern clades. Furthermore, during the BIOSPEEDO cruise at least 10 still unnamed species were collected between 7°25′ S and 21°33′ S. The shift in community structure identified by MRT analysis was located south of 17°34′ S or south of 13°59′ S, depending on the data used, suggesting that the southern part of the SEPR (17°25′–21°33′ S) constitutes a biogeographic transition zone in the vent fauna along the EPR. At a regional scale, latitude combined with the type of venting was significantly correlated with the community structure associated with mussel beds. Main conclusions Together, the molecular data, in situ observations, and the distribution of species suggest that the high diversity of vent fauna species presently observed between 17°25′ S and 21°33′ S is probably a result of the overlap of several distinct biogeographic provinces. We argue that this area thus constitutes a biogeographic vent fauna transition zone along the EPR.