Martin B. Hebsgaard
University of Copenhagen
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Featured researches published by Martin B. Hebsgaard.
Systematic Biology | 2009
Mette E. Steeman; Martin B. Hebsgaard; R. Ewan Fordyce; Simon Y. W. Ho; Daniel L. Rabosky; Rasmus Nielsen; Carsten Rahbek; Henrik Glenner; Martin V. Sørensen
Abstract The remarkable fossil record of whales and dolphins (Cetacea) has made them an exemplar of macroevolution. Although their overall adaptive transition from terrestrial to fully aquatic organisms is well known, this is not true for the radiation of modern whales. Here, we explore the diversification of extant cetaceans by constructing a robust molecular phylogeny that includes 87 of 89 extant species. The phylogeny and divergence times are derived from nuclear and mitochondrial markers, calibrated with fossils. We find that the toothed whales are monophyletic, suggesting that echolocation evolved only once early in that lineage some 36–34 Ma. The rorqual family (Balaenopteridae) is restored with the exclusion of the gray whale, suggesting that gulp feeding evolved 18–16 Ma. Delphinida, comprising all living dolphins and porpoises other than the Ganges/Indus dolphins, originated about 26 Ma; it contains the taxonomically rich delphinids, which began diversifying less than 11 Ma. We tested 2 hypothesized drivers of the extant cetacean radiation by assessing the tempo of lineage accumulation through time. We find no support for a rapid burst of speciation early in the history of extant whales, contrasting with expectations of an adaptive radiation model. However, we do find support for increased diversification rates during periods of pronounced physical restructuring of the oceans. The results imply that paleogeographic and paleoceanographic changes, such as closure of major seaways, have influenced the dynamics of radiation in extant cetaceans.
Proceedings of the National Academy of Sciences of the United States of America | 2007
Sarah Stewart Johnson; Martin B. Hebsgaard; Torben R. Christensen; Mikhail Mastepanov; Rasmus Nielsen; Kasper Munch; Tina B. Brand; Mark G. Thomas; P. Gilbert; Maria T. Zuber; Michael Bunce; Regin Rønn; David A. Gilichinsky; Duane G. Froese
Recent claims of cultivable ancient bacteria within sealed environments highlight our limited understanding of the mechanisms behind long-term cell survival. It remains unclear how dormancy, a favored explanation for extended cellular persistence, can cope with spontaneous genomic decay over geological timescales. There has been no direct evidence in ancient microbes for the most likely mechanism, active DNA repair, or for the metabolic activity necessary to sustain it. In this paper, we couple PCR and enzymatic treatment of DNA with direct respiration measurements to investigate long-term survival of bacteria sealed in frozen conditions for up to one million years. Our results show evidence of bacterial survival in samples up to half a million years in age, making this the oldest independently authenticated DNA to date obtained from viable cells. Additionally, we find strong evidence that this long-term survival is closely tied to cellular metabolic activity and DNA repair that over time proves to be superior to dormancy as a mechanism in sustaining bacteria viability.
Systematic Entomology | 2004
Martin B. Hebsgaard; Nils Møller Andersen; Jakob Damgaard
Abstract. Morphological characters and molecular sequence data were for the first time analysed separately and combined for the true water bugs (Hemiptera–Heteroptera, infraorder Nepomorpha). Data from forty species representing all families were included, together with two outgroup species representing the infraorders Gerromorpha and Leptopodomorpha. The morphological data matrix consisted of sixty‐five characters obtained from literature sources. Molecular data included approximately 960 bp from the mitochondrial gene 16S and the nuclear gene 28S for all forty‐two terminal taxa. The morphological dataset was analysed using maximum parsimony and the combined morphological and molecular (16S + 28S rDNA) dataset was analysed using direct optimization. A sensitivity analysis of sixteen different sets of parameters (various combinations of insertion–deletion cost and transversion costs) was undertaken. Character congruence was used as an optimality criterion to choose among competing phylogenetic hypotheses. The final hypothesis was obtained from the analysis of the combined molecular and mor phological dataset with the most congruent parameter set. This hypothesis supports the monophyly of all currently recognized families of Nepomorpha, and of the superfamilies Nepoidea (Nepidae + Belostomatidae), Corixoidea (Corixidae), Ochteroidea Ochteridae + Gelastocoridae), Notonectoidea (Notonectidae), and Pleoidea (Pleidae + Helotrephidae), but not the monophyly of the Naucoroidea (Naucoridae + Aphelocheiridae + Potamocoridae). The close relationship between the Notonectidae and Pleoidea is also supported. Our hypothesis concurs with Mahner in the placement of the Corixidae as a sister group to the remaining nepomorphan superfamilies except the Nepoidea, but differs in the placement of the Ochteroidea as a sister group to the Notonectoidea + Pleoidea. The superfamily Naucoroidea should be limited to only including the family Naucoridae and not the families Aphelocheiridae and Potamocoridae. The present analysis strongly supports a sister group relationship between the families Aphelocheiridae and Potamocoridae, a monophylum for which we propose a new superfamily, Aphelocheiroidea.
Antiquity | 2009
Martin B. Hebsgaard; M. Thomas P. Gilbert; Jette Arneborg; Patricia Heyn; Morten E. Allentoft; Michael Bunce; Kasper Munch; Charles E. Schweger
Abstract It is probable that ‘The Farm Beneath the Sand’ will come to stand for a revolution in archaeological investigation. The authors show that a core of soil from an open field can provide a narrative of grazing animals, human occupation and their departure, just using DNA and AMS dating. In this case the conventional archaeological remains were nearby, and the sequence obtained by the old methods of digging and faunal analysis correlated well with the story from the core of ancient ‘dirt’ DNA. The potential for mapping the human, animal and plant experience of the planet is stupendous.
Journal of Molecular Evolution | 2007
Martin B. Hebsgaard; Carsten Wiuf; M. Thomas P. Gilbert; Henrik Glenner
The retrieval of Neanderthal (Homo neanderthalsensis) mitochondrial DNA is thought to be among the most significant ancient DNA contributions to date, allowing conflicting hypotheses on modern human (Homo sapiens) evolution to be tested directly. Recently, however, both the authenticity of the Neanderthal sequences and their phylogenetic position outside contemporary human diversity have been questioned. Using Bayesian inference and the largest dataset to date, we find strong support for a monophyletic Neanderthal clade outside the diversity of contemporary humans, in agreement with the expectations of the Out-of-Africa replacement model of modern human origin. From average pairwise sequence differences, we obtain support for claims that the first published Neanderthal sequence may include errors due to postmortem damage in the template molecules for PCR. In contrast, we find that recent results implying that the Neanderthal sequences are products of PCR artifacts are not well supported, suffering from inadequate experimental design and a presumably high percentage (>68%) of chimeric sequences due to “jumping PCR” events.
Archive | 2009
Martin B. Hebsgaard
The DNA molecule degrades over time, just like other cellular components if not repaired. Often the degradation is relatively fast, as fossil remains that are only a few hundred years old contain little or no amplifiable endogenous DNA. One basic question in research on ancient DNA is “how long can DNA and cells survive?” This question is not easily answered because it depends on numerous interacting factors. A maximum DNA survival of 50,000–1 million years has been suggested from theoretical considerations and empirical studies. It is clear that temperature is an important factor, because low temperatures and dry conditions slow the rate of chemical processes that degrade DNA. Given that rates of reaction generally drop an order of magnitude for every 10°C drop in temperature, colder environments are naturally better environments for long-term storage of DNA (Smith et al. 2001). Other natural processes that accelerate the degradation of the DNA molecule are endogenous and exogenous nucleases, as well as hydrolysis (Lindahl 1993; Handt et al. 1994; Hofreiter et al. 2001a). Despite the predicted maximum age of DNA, several studies have claimed to be able to extract DNA many million of years old, yet others fail to amplify DNA with a very young origin. How do we explain this discrepancy? On the one hand, we know that DNA degrades over time and that fossil remains can contain very little or no DNA. This is a problematic situation, which makes the studies very prone to contamination, giving false-positive results.
Science | 2007
Enrico Cappellini; Wouter Boomsma; Rasmus Nielsen; Martin B. Hebsgaard; Tina B. Brand; Michael Hofreiter; Michael Bunce; Hendrik N. Poinar; Dorthe Dahl-Jensen; Sigfus J Johnsen; Jørgen Peder Steffensen; Ole Bennike; Jean-Luc Schwenninger; Roger Nathan; Simon J. Armitage; Cees-Jan de Hoog; Vasily Alfimov; Marcus Christl; Juerg Beer; Raimund Muscheler; J. D. Barker; Martin Sharp; Kirsty Penkman; James Haile; Pierre Taberlet; M. Thomas P. Gilbert; Antonella Casoli; Elisa Campani; Matthew J. Collins
Science | 2006
Henrik Glenner; Philip Francis Thomsen; Martin B. Hebsgaard; Martin V. Sørensen
Trends in Microbiology | 2005
Martin B. Hebsgaard; Matthew J. Phillips
Journal of Zoological Systematics and Evolutionary Research | 2008
Martin V. Sørensen; Martin B. Hebsgaard; Iben Heiner; Henrik Glenner; Reinhardt Møbjerg Kristensen