Phylogenomische Untersuchungen zur Aufklärung des Metazoa-Stammbaums

Zentrales Thema der Arbeit war die Aufklärung von Verwandtschaftsverhältnissen im „Tree of Life“ der vielzelligen Tiere (Metazoa) unter Einsatz großer DNA-Sequenzdatensätze und phylogenomischer Methoden. Zur Untersuchung der internen Phylogenie der Syndermata (= meist freilebende Rädertiere („Rotifera“) + endoparasitische Kratzwürmer (Acanthocephala)) sowie ihrer Position im Metazoen-Stammbaum wurden insgesamt sieben neue mitochondriale (mt) Genome sowie neue Transkriptom-Sequenzdaten von sieben verschiedenen Syndermata-Spezies generiert und/oder analysiert. Die Stammbaumrekonstruktionen auf Grundlage dieser sowie orthologer Sequenzen anderer Spezies in Form von phylogenomischen Datensätzen mit bis zu 82.000 Aminosäurepositionen ergaben folgende Aussagen zur Evolution: (i) Innerhalb der Acanthocephala bilden monophyletische Palaeacanthocephala das Schwestertaxon zu den Eoacanthocephala. Die Archiacanthocephala sind Schwestertaxon zu allen vorgenannten. (ii) Innerhalb der Syndermata bilden die epizoisch lebenden Seisonidea das Schwestertaxon zu den endoparasitischen Acanthocephala (= Pararotatoria), die Bdelloidea sind das Schwestertaxon zu den Pararotatoria (= Hemirotifera) und die Monogononta das Schwestertaxon zu den Hemirotifera. Die klassischen Eurotatoria (= Bdelloidea + Monogononta) sind demnach paraphyletisch. (iii) Innerhalb der Metazoa bilden die Syndermata gemeinsam mit den Gnathostomulida die Gnathifera. Diese sind die Schwestergruppe zu allen anderen Spiralia-Taxa, welche sich in Rouphozoa (= Platyhelminthes + Gastrotricha) sowie die Lophotrochozoa aufspalten. Die Platyzoa (= Gnathifera + Platyhelminthes + Gastrotricha) sind demnach paraphyletisch. Diese phylogenetischen Hypothesen wurden im Hinblick auf ihre Implikationen für die Evolution morphologischer und ökologischer Merkmale interpretiert. Demnach sind während der Evolution dieser Tiergruppen mehrfach sekundäre Verlustereignisse von komplexen morphologischen Merkmalen aufgetreten (laterale sensorische Organe innerhalb der Acanthocephala und das Räderorgan (Corona) innerhalb der Syndermata), was die Verwendung dieser Merkmale im Sinne einer klassisch-morphologischen Phylogenetik kritisch erscheinen lässt. Der Endoparasitismus der Acanthocephala hat sich wahrscheinlich über ein epizoisches Zwischenstadium, wie man es heute noch bei den Seisonidea findet, entwickelt. Der letzte gemeinsame Vorfahre der Spiralia war vermutlich klein und unsegmentiert und besaß keine echte Leibeshöhle (Coelom). Demnach hätten sich Segmentierung und Coelome innerhalb der Metazoa mehrfach unabhängig voneinander (konvergent) entwickelt. Die Arbeit beinhaltete folgende weitere, zum Teil methodische Aspekte: (i) die Analyse der Architektur der mt Genome der Monogononta bestätigte die aberrante Organisation in zwei Subgenomen für die Brachionidae. (ii) Eine Prüfung der Tauglichkeit ribosomaler Proteine für molekular-phylogenetische Arbeiten ergab das Vorhandensein widersprüchlicher phylogenetischer Signale in diesen speziellen Proteinsequenzen. (iii) Es konnte nachgewiesen werden, dass systematische Fehler wie „long-branch attraction“ bei der Positionierung der Syndermata im Stammbaum der Metazoa eine große Rolle spielen und adressiert werden müssen.

Did homeodomain proteins duplicate before the origin of angiosperms, fungi, and metazoa?

Homeodomain proteins are transcription factors that play a critical role in early development in eukaryotes. These proteins previously have been classified into numerous subgroups whose phylogenetic relationships are unclear. Our phylogenetic analysis of representative eukaryotic sequences suggests that there are two major groups of homeodomain proteins, each containing sequences from angiosperms, metazoa, and fungi. This result, based on parsimony and neighbor-joining analyses of primary amino acid sequences, was supported by two additional features of the proteins. The two protein groups are distinguished by an insertion/deletion in the homeodomain, between helices I and II. In addition, an amphipathic alpha-helical secondary structure in the region N terminal of the homeodomain is shared by angiosperm and metazoan sequences in one group. These results support the hypothesis that there was at least one duplication of homeobox genes before the origin of angiosperms, fungi, and metazoa. This duplication, in turn, suggests that these proteins had diverse functions early in the evolution of eukaryotes. The shared secondary structure in angiosperm and metazoan sequences points to an ancient conserved functional domain.

Evolution of duplicate control regions in the mitochondrial genomes of metazoa: A case study with Australasian Ixodes ticks

To investigate the evolution pattern and phylogenetic utility of duplicate control regions (CRs) in mitochondrial (mt) genomes, we sequenced the entire mt genomes of three Ixodes species and part of the mt genomes of another I I species. All the species from the Australasian lineage have duplicate CRs, whereas the other species have one CR. Sequence analyses indicate that the two CRs of the Australasian Ixodes ticks have evolved in concert in each species. In addition to the Australasian Ixodes ticks, species from seven other lineages of metazoa also have mt genomes with duplicate CRs. Accumulated mtDNA sequence data from these metazoans and two recent experiments on replication of mt genomes in human cell lines with duplicate CRs allowed us to re-examine four intriguing questions about the presence of duplicate CRs in the mt genomes of metazoa: (1) Why do some mt genomes, but not others, have duplicate CRs? (2) How did mt genomes with duplicate CRs evolve? (3) How could the nucleotide sequences of duplicate CRs remain identical or very similar over evolutionary time? (4) Are duplicate CRs phylogenetic markers? It appears that mt genomes with duplicate CRs have a selective advantage in replication over mt genomes with one CR. Tandem duplication followed by deletion of genes is the most plausible mechanism for the generation of mt genomes with duplicate CRs. Once duplicate CRs occur in an mt genome, they tend to evolve in concert, probably by gene conversion. However, there are lineages where gene conversion may not always occur, and, thus, the two CRs may evolve independently in these lineages. Duplicate CRs have much potential as phylogenetic markers at low taxonomic levels, such as within genera, within families, or among families, but not at high taxonomic levels, such as among orders.

Surface characteristics and metazoa occurrence at ice station PS67/006-1 during POLARSTERN cruise ANT-XXII/2 (Nov 2004-Jan 2005)

The surface and sub-ice layer habitats and their metazoan fauna were studied on a drifting pack-ice floe in the western Weddell Sea from 29 November 2004 to 1 January 2005 during the "Ice Station POLarstern" (ISPOL). Flooding of the floe occurred at some places, and the establishment of surface layers with a brownish colour due to growing algae was observed at several sampling sites. The average surface-layer temperature, brine salinity and brine volume were -1.4 °C, 25.3 and 54%, respectively. The temperature-salinity relationship in the surface layer was seldom at equilibrium conditions. Chlorophyll a (Chl a) concentrations in the brine varied between 1.0 and 53.5 µg /L. Surface-layer thickness, salinity, Chl a concentration and copepod abundances were generally higher at the edge of the floe than in the inner part. The sympagic copepod species Drescheriella glacialis/racovitzai and Stephos longipes, with abundances ranging between 0 and 3830 ind/L (median: 2 ind/L) and 0 and 1293 ind/L (median: 4 ind/L), respectively, were the dominant members of the surface-layer meiofauna. Their populations consisted mainly of adults and early naupliar stages, which points to an active reproduction of these species within the surface layer. Other taxa found in the surface layer were undetermined turbellarians, the gastropod Tergipes antarcticus, and, for the first time, the ctenophore Callianira antarctica, and the amphipods Eusirus antarcticus and Eusirus tridentatus. During the course of our study, slight melting at the ice underside took place, releasing sympagic organisms to the water column. Chl a concentrations in the sub-ice water layer were very low (0.1-0.5 µg /L), except for 25 December when the Chl a concentration at 0 m depth increased to 2.3 µg /L. The most dominant sympagic copepod species found in the sub-ice layer was Ectinosoma sp., with abundances ranging between 1 and 599 ind/m**3 (median: 25 ind/m**3). Other sympagic copepod species occurring regularly in this habitat were D. glacialis/racovitzai, Diarthrodes cf. lilacinus, Idomene antarctica and S. longipes. All of these sympagic species were generally found in higher abundances at 0 m depth underneath the ice than at 5 m depth, in contrast to pelagic copepod species that occurred more frequently at 5 m depth. Niche separation and probable life-cycle strategies of dominant sympagic metazoans are discussed.

The ancient gene C12orf29 : an exploration of its role in the chordate body plan

The sheep (Ovis aries) is commonly used as a large animal model in skeletal research. Although the sheep genome has been sequenced there are still only a limited number of annotated mRNA sequences in public databases. A complementary DNA (cDNA) library was constructed to provide a generic resource for further exploration of genes that are actively expressed in bone cells in sheep. It was anticipated that the cDNA library would provide molecular tools for further research into the process of fracture repair and bone homeostasis, and add to the existing body of knowledge. One of the hallmarks of cDNA libraries has been the identification of novel genes and in this library the full open reading frame of the gene C12orf29 was cloned and characterised. This gene codes for a protein of unknown function with a molecular weight of 37 kDa. A literature search showed that no previous studies had been conducted into the biological role of C12orf29, except for some bioinformatics studies that suggested a possible link with cancer. Phylogenetic analyses revealed that C12orf29 had an ancient pedigree with a homologous gene found in some bacterial taxa. This implied that the gene was present in the last common eukaryotic ancestor, thought to have existed more than 2 billion years ago. This notion was further supported by the fact that the gene is found in taxa belonging to the two major eukaryotic branches, bikonts and unikonts. In the bikont supergroup a C12orf29-like gene was found in the single celled protist Naegleria gruberi, whereas in the unikont supergroup, encompassing the metazoa, the gene is universal to all chordate and, therefore, vertebrate species. It appears to have been lost to the majority of cnidaria and protostomes taxa; however, C12orf29-like genes have been found in the cnidarian freshwater hydra and the protostome Pacific oyster. The experimental data indicate that C12orf29 has a structural role in skeletal development and tissue homeostasis, whereas in silico analysis of the human C12orf29 promoter region suggests that its expression is potentially under the control of the NOTCH, WNT and TGF- developmental pathways, as well SOX9 and BAPX1; pathways that are all heavily involved in skeletogenesis. Taken together, this investigation provides strong evidence that C12orf29 has a very important role in the chordate body plan, in early skeletal development, cartilage homeostasis, and also a possible link with spina bifida in humans.

Temporal and spacial control of RNA stability in the early embryo of Drosophila melanogaster

Early embryogenesis in metazoa is controlled by maternally synthesized products. Among these products, the mature egg is loaded with transcripts representing approximately two thirds of the genome. A subset of this maternal RNA pool is degraded prior to the transition to zygotic control of development. This transfer of control of development from maternal to zygotic products is referred to as the midblastula transition (or MBT). It is believed that the degradation of maternal transcripts is required to terminate maternal control of development and to allow zygotic control of development to begin. Until now this process of maternal transcript degradation and the subsequent timing of the MBT has been poorly understood. I have demonstrated that in the early embryo there are two independent RNA degradation pathways, either of which is sufficient for transcript elimination. However, only the concerted action of both pathways leads to elimination of transcripts with the correct timing, at the MBT. The first pathway is maternally encoded, is triggered by egg activation, and is targeted to specific classes of mRNAs through cis-acting elements in the 3' untranslated region (UTR}. The second pathway is activated 2 hr after fertilization and functions together with the maternal pathway to ensure that transcripts are degraded by the MBT. In addition, some transcripts fail to degrade at select subcellular locations adding an element of spatial control to RNA degradation. The spatial control of RNA degradation is achieved by protecting, or masking, transcripts from the degradation machinery. The RNA degradation and protection events are regulated by distinct cis-elements in the 3' untranslated region (UTR). These results provide the first systematic dissection of this highly conserved process in development and demonstrate that RNA degradation is a novel mechanism used for both temporal and spatial control of development.

A simple method for counting bacteria with active electron transport system in water and sediment samples [Translation from: Kiel. Meeresforsch. 31(2) 83-86, 1975]

Description of a simple method for counting bacteria with active electron transport systems in water and sediment samples. Sodium succinate, NADH and NADPH served as electron donors. It is possible to see several sites of electron transport in the larger cells. Especially impressive are the plankton-algae, protozoa, and small metazoa. This is a partial translation of the ”method” section only.