Weitere biologische Literatur (eingeschränkter Zugriff)
Refine
Year of publication
- 2007 (23) (remove)
Document Type
- Doctoral Thesis (12)
- Article (10)
- Part of a Book (1)
Language
- English (23) (remove)
Has Fulltext
- yes (23)
Is part of the Bibliography
- no (23)
Keywords
- taxonomy (3)
- distribution (2)
- phylogeny (2)
- ABC-Transporter (1)
- Ackerschmalwand (1)
- Alpha-Bungarotoxin (1)
- Asien (1)
- Blutgefäß (1)
- Blutgefäßsystem (1)
- Bungarus (1)
Institute
- Biochemie und Chemie (7)
- Biowissenschaften (5)
- Extern (3)
Shaped by some of the most dramatic tectonic events of the Cenozoic, the parts of southern and eastern Asia that have become known as the Oriental faunal region comprise vast areas of great geological complexity and ecological diversity. One of the four major groups of terrestrial elapid snakes in this region is the genus Bungarus. These nocturnal and predominantly ophiophagous snakes are widely known as kraits and are an important cause of snakebite mortality throughout their wide range that extends from Afghanistan to Vietnam and eastern China, and south to the Indonesian islands of Java and Bali. Although present on Borneo, kraits have not been found on any island of the Philippines, nor on Lesser Sunda Islands east of Bali. Despite their medical significance and the great importance of Bungarus toxins as tools in neuropharmacology, krait systematics and taxonomy have remained largely unstudied. Twelve species of Bungarus were recognized at the beginning of the present study. Many of these are rare in collections, and most aspects of their biology are unknown. While some species are highly distinct, most kraits are conservative morphologically, rendering molecular methods invaluable for the study of their diversity and biogeography. This study is the first to address the relationships within Bungarus and the historical biogeography of kraits based on molecular evidence. I inferred phylogeographic relationships based on analyses of new nucleotide sequences of the entire mitochondrial cytochrome b gene of 51 kraits and partial NADH dehydrogenase subunit 4 sequences of 40 kraits which I analyzed together with a representative sample of 32 published elapid and non-elapid outgroup taxa using Bayesian, maximum-likelihood, maximum-parsimony and neighbor-joining methods. I then used the recovered phylogeny to investigate the evolution of selected morphological characters and, together with collections-based geographical distribution information, in dispersal-vicariance analyses with models of variable taxonomic and biogeographic complexity. The phylogenetic analyses demonstrate that the current taxonomy of kraits does not adequately represent either the relationships or the genetic diversity in this genus. In contrast, I identified monophyletic groups that are congruent with recognized biogeographic units as well as extensive ecomorph evolution and morphologically cryptic speciation. The following additional conclusions are collectively supported by the mitochondrial phylogeny and morphological as well as biochemical synapomorphies: (1) Kraits are monophyletic with respect to the remaining taxa of the Elapidae; (2) Bungarus flaviceps and Bungarus bungaroides form the monophyletic sister clade of a clade formed by B. fasciatus, black-and-white-banded, and uniformly black taxa; (3) the remaining taxa are divisible into two sister clades, the South Asian species (Bungarus sindanus (Bungarus caeruleus, Bungarus ceylonicus)) vs. Himalayan, Burmese, Southeast and East Asian taxa; (4) within the latter, Burmese taxa form the sister clade to Southeast and East Asian taxa; (5) the widespread and medically significant species Bungarus candidus and Bungarus multicinctus are paraphyletic. The results of this study highlight the importance of vicariant geological events and sea level fluctuations for the cladogenesis of kraits. Events of particular importance in the evolution of kraits include the uplift of the Indo-Burman ranges (Arakan-Naga Hills) which separated black-and-white banded kraits in India and Southeast Asia, and the uplift of mountain ranges in Yunnan, China (e.g., the Gaoligong Shan), which coincided with lineage separation in two distantly related clades of kraits. Alternating dispersal and vicariance events due to Pleistocene climatic and sea level changes have caused complex phylogeographic patterns in kraits in Southeast Asia. Zones of contact between closely related evolutionary lineages of the B. candidus complex are identified in Thailand, Vietnam, and southern China (Hainan). Within this complex, two main clades are revealed. One includes populations from the Southeast Asian mainland and is in contact with B. multicinctus in southern China. The other consists of populations from Thailand, southern Vietnam, Java, and Bali. The phylogeny as well as genetic distances suggest a scenario in which a Pleistocene southward dispersal of B. candidus to Sumatra, Java, and Bali during times of low sea levels was temporarily interrupted by vicariant events (rising sea levels, especially flooding of the Malacca Strait between Sumatra and the Malay Peninsula, and of the Bali Strait between Java and Bali). In this context, the close phylogenetic relationship between haplotypes from southern Vietnam and those from Java and Bali suggests that "southern" B. candidus dispersed directly via colonization of the widely receded South Chinese Sea, and not by taking a detour via the Malay Peninsula and Thailand, which were already inhabited by other populations of B. candidus. Using these phylogenetic estimates as the framework for a study on the diversity and evolution of krait venom components, I applied biochemical and molecular genetic approaches to identify and quantify polypeptide and protein toxins in krait venom, focusing on the distribution and molecular evolution of alpha-bungarotoxin, an irreversible competitive antagonist of nicotinic acetylcholine receptors with an exceptionally high applied significance as a receptor probe. I was specifically interested in the medically relevant question of intraspecific and interspecific variability in toxin diversity, and whether receptor-binding postsynaptic toxins evolve at rates different from those of presynaptic neurotoxins like beta-bungarotoxin, which act by destroying the nerve terminal and are believed to exhibit hypervariable functional diversification due to an accelerated mode of molecular evolution. In the context of this question, I isolated and purified the major lethal neurotoxins from B. candidus venoms by sequential steps of liquid chromatography for structural and functional characterization studies. Cloning and sequence analysis of toxin-coding genomic DNAs showed that the gene encoding the alpha-bungarotoxin alanine-31 variant, originally isolated from B. multicinctus venom, is widely present and highly conserved in multiple populations of B. candidus and is expressed as the principal postsynaptic neurotoxin at least in Javan B. candidus. In addition to the widespread presence of genomic DNAs encoding the alpha-bungarotoxin alanine-31 variant, the present study also revealed the partial genes of three novel alpha-bungarotoxin isoforms in addition to the previously known alanine-31 and valine-31 variants, all of which share an invariant exon 3 coding region. While alpha-bungarotoxin is the principal postsynaptic neurotoxin of Taiwanese B. multicinctus and Javan B. candidus, the main postsynaptic neurotoxin of Thai B. candidus both by quantity and lethality was a novel polypeptide of similar toxicity with a mass of 8030 Da and 73 amino acid residues, whose characterization at the genetic and protein levels revealed a novel subgroup of krait neurotoxins, here named alpha-delta-bungarotoxins and represented by four sequences from Bungarus caeruleus and B. candidus. alpha-delta-Bungarotoxins share high sequence homology with alpha-bungarotoxins but the purified, 8030 Da alpha-delta-bungarotoxin-1 exhibits only reversible, low affinity binding to nicotinic receptors and high site-selectivity for the acetylcholine binding site at the alpha-delta-subunit interface of the receptor. These properties render alpha-delta-bungarotoxin not only the first snake long-chain neurotoxin with reversible binding and binding-site selectivity, but also an exciting natural tool with which to address structure-function relationships at the subunit interfaces of the human receptor. The results of comparisons of the number of non-synonymous nucleotide substitutions per nonsynonymous site (dN) to the number of synonymous nucleotide substitutions per synonymous site (dS) strongly suggest that positive selection is acting on exon 2 of the alpha-bungarotoxin and probably also of the alpha-delta-bungarotoxin genes. In addition, the numbers of nucleotide substitutions per site of intron (dI) compared to the dS value of the toxin-coding exon regions provide strong evidence for accelerated molecular evolution in exon 2 of alpha-delta-bungarotoxins —whose value of dI is only one-eighth of the value of dS—whereas the hypothesis of accelerated evolution is rejected for 13 unique genomic DNAs encoding five alpha-bungarotoxin isoforms from B. candidus and B. multicinctus....
Glyptostrobus Endlicher is well represented in early Early Cretaceous to Pleistocene deposits in the middle to high latitudes of North America and Eurasia. Although the taxonomy and nomenclature of the genus is complicated, the fossil record indicates Glyptostrobus was represented by a small number of species. The genus first appears in Aptian age deposits from western Canada and Greenland, and achieved a wide distribution early in its evolutionary history. Exchange of Glyptostrobus between Asia and North America occurred across the Spitsbergen and Beringian corridors, which were functional about 110 and 100 million years ago, respectively The Late Cretaceous fossil record of Glyptostrobus shows that the genus had spread into Russia, China and the shores of the Turgai Strait. By the early Tertiary, Glyptostrobus was a prominent constituent of the polar broad-leaved deciduous forests. Paleocene age deposits across western Canada and the United States indicate the genus was present in great abundance in the lowland warm temperate and subtropical forests east of the Rocky Mountains. The broad distribution in North America and Russia during the Paleocene and Eocene indicates that Glyptostrobus grew and reproduced under a diverse range of climatic and environmental conditions, including the cold and unique lighting conditions of the polar latitudes. The presence of Glyptostrobus in Europe indicates the North Atlantic land bridges that extended between North America and Eurasia (Fennoscandia) and Europe during the early Tertiary were used. In Europe, extensive Glyptostrobus dominated swan1ps occupied the Central European Depression during the late Tertiary. Increasing global aridity and cooling, as well as landscape stabilization together with increasing competition for resources and habitat by representatives of the Pinaceae, seem to have forced the genus out of North America, Europe and most of Asia during the Miocene and Pliocene. In Japan, Glyptostrobus persisted until the early Pleistocene. After the early Pleistocene extinction in Japan, Glyptostrobus reappeared in southeastern China. Details of the taxonomic and biogeographic history of Glyptostrobus are examined.
The chemiosmotic theory suggested by Peter Mitchell (Mitchell, 1961, Nature 191:144-148; see Mitchell, 1979, Science 206:1148-1159 for review) postulated that the energy released upon the oxidation of electron donor substrates is transiently stored as electrochemical proton potential, delta-p across energy-transducing membranes, which acts then as the driving force for the ATP synthesis. Membrane protein complexes can both generate and utilise a transmembrane electrochemical proton potential, either by transmembrane proton transfer or by transmembrane electron transfer coupled to protolytic reactions on opposite sides of the membrane. The dihaem-containing membrane protein complex quinol:fumarate reductase (QFR) from the anaerobic epsilon-proteobacterium Wolinella succinogenes apparently combines both of these mechanisms (Haas et al, 2005, Biochemistry 44:13949-13961; Lancaster et al, 2005, PNAS 102:18860–18865; Mileni et al, 2005, Biochemistry 44:16718-16728; Madej et al, 2006, EMBO J 25:4963-4970). QFR is the terminal enzyme of anaerobic fumarate respiration that allows bacteria to use fumarate as the terminal electron acceptor (Kröger, 1978, Biochim Biophys Acta 505:129-45; Lancaster, 2004, In: Respiration in Archaea and Bacteria Volume 1:57-85). QFR couples the two-electron reduction of fumarate to succinate to the two-electron oxidation of quinol to quinone. QFR contains two haem b groups bound by the transmembrane subunit C, which are termed the ‘proximal haem’, bP, and the ‘distal haem’, bD, according to the relative proximity to the hydrophilic subunits A and B (Lancaster et al, 1999, Nature 402:377-85). The two-electron transfer via the two haem groups has been proposed (Lancaster, 2002, Biochimica et Biophysica Acta 1565:215-231) and demonstrated (Madej et al, 2006, EMBO J 25:4963-4970) to be coupled to a compensatory, parallel transfer of two protons via a transmembrane proton transfer pathway. The two most prominent constituents of the proposed pathway were suggested to be the haem bD ring C propionate and the side chain of amino-acid residue Glu C180, after which the proton transfer pathway was named the ‘E-pathway’ (Lancaster, 2002, Biochimica et Biophysica Acta 565:215-231). The essential role of Glu C180 was supported by site-directed mutagenesis and structural and functional characterization of the enzyme E180Q, where the Glu C180 was replaced with a Gln residue (Lancaster et al, 2005, PNAS 102:18860–18865). Moreover, multiconformer continuum electrostatics (MCCE) calculations (Haas and Lancaster 2004, Biophys J 87:4298-4315) and Fouriertransformed infrared (FTIR) spectroscopy experiments (Haas et al, 2005, Biochemistry 44:13949-13961) indicated the Glu C180 side chain to undergo a combination of a conformational change and protonation upon haem reduction. The contribution of haem bD propionate is less clear, however, a combination of 13C labelling of the haem propionates with redox-induced FTIR experiments (Mileni et al, 2005, Biochemistry 44:16718-16728) and MCCE calculations (Haas and Lancaster, 2004, Biophys J 87:4298-4315) support a change in protonation, possibly accompanied by a change in environment upon haem reduction. These experiments and their results strongly support the existence of the ‘E-pathway’ which is transiently open during the reduction of the haem groups and blocked in the oxidized state of the enzyme (Lancaster, 2002b, Biochim Biophys Acta 1565:215-231). All available crystal structures of the QFR, however, are those of the oxidized enzyme. Therefore, it is advantageous to perform simulations of various redox states of the enzyme to determine for instance, how the side-chain of Glu C180 and haem bD ring C propionate behave upon changes of the redox states of the haem groups and why is the ‘E-pathway’ blocked in the oxidized state of the enzyme. Although the distal haem ring C propionate and Glu C180 were identified as the most prominent components of the proton transfer pathway, it was not clear, on the basis of the structure, how proton transfer could occur between them. In addition, two constituents are not enough to span the membrane region and the additional participants in the proton transfer pathway must be identified. Since an atomistic investigation of proton transfer in this system is not yet possible experimentally, I used available theoretical methods such as classical molecular dynamics (MD) simulation (Alder and Wainwright, 1959, J Phys Chem 31:459-466; McCammon et al, 1977, Nature 267:585-590) and Q-HOP molecular dynamics (Q-HOP MD) simulation (Lill and Helms, 2001, J Chem Phys 115:7993-8005) to investigate the postulated mechanism of electron coupled proton transfer in QFR. MD simulations allowed us to move away from static difference pictures obtained from FTIR experiments and MCCE calculations. The advantage of the MD simulations over the experiments and the simulations performed so far is that the time-dependent properties could now be analyzed. The behaviour of various residues and their side-chains and any environmental changes may be directly observed during MD simulations. Although classical MD simulations cannot be used to study proton transfer reactions, they can provide information on formation of configurations that would allow either direct proton transfer between donor and acceptor residues or indirect proton transfer mediated by water molecules. To avoid the static protonation of residues which is inherent in classical MD simulations, Q-HOP MD simulations were performed which explicitly describe proton transfer reactions by allowing the change of the protonation state of residues ‘on the fly’. The structures obtained after classical molecular dynamics simulations ....