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PubMed2002

Mantle compensation of active metamorphic core complexes at Woodlark rift in Papua New Guinea.

In many highly extended rifts on the Earth, tectonic removal of the upper crust exhumes mid-crustal rocks, producing metamorphic core complexes. These structures allow the upper continental crust to accommodate tens of kilometres of extension, but it is not clear how the lower crust and underlying mantle respond. Also, despite removal of the upper crust, such core complexes remain both topographically high and in isostatic equilibrium. Because many core complexes in the western United States are underlain by a flat Moho discontinuity, it has been widely assumed that their elevation is supported by flow in the lower crust or by magmatic underplating. These processes should decouple upper-crust extension from that in the mantle. In contrast, here we present seismic observations of metamorphic core complexes of the western Woodlark rift that show the overall crust to be thinned beneath regions of greatest surface extension. These core complexes are actively being exhumed at a rate of 5-10 km Myr(-1), and the thinning of the underlying crust appears to be compensated by mantle rocks of anomalously low density, as indicated by low seismic velocities. We conclude that, at least in this case, the development of metamorphic core complexes and the accommodation of high extension is not purely a crustal phenomenon, but must involve mantle extension.

Journal Article↗

PubMed2005

Orogeny can be very short.

In contrast to continent/continent collision, arc-continent collision generates very short-lived orogeny because the buoyancy-driven impedance of the subduction of continental lithosphere, accompanied by arc/suprasubduction-zone ophiolite obduction, is relieved by subduction polarity reversal (flip). This tectonic principle is illustrated by the early Ordovician Grampian Orogeny in the British and Irish Caledonides, in which a wealth of detailed sedimentologic, heavy mineral, and geochronologic data pin the Orogeny to a very short Arenig/Llanvirn event. The Orogeny, from the initial subduction of continental margin sediments to the end of postflip shortening, lasted approximately 18 million years (my). The collisional shortening, prograde-metamorphic phase of the Orogeny lasted 8 my, extensional collapse and exhumation of midcrustal rocks lasted 1.5 my, and postflip shortening lasted 4.5 my. Strain rates were a typical plate-boundary-zone 10(-15). Metamorphism, to the second sillimanite isograd, with extensive partial melting, occurred within a few my after initial collision, indicating that conductive models for metamorphic heat transfer in Barrovian terrains are incorrect and must be replaced by advective models in which large volumes of mafic/ultramafic magma are emplaced, syn-tectonically, below and into evolving nappe stacks. Arc/continent collision generates fast and very short orogeny, regional metamorphism, and exhumation.

Journal Article↗

PubMed2005

Stability of ferruginous bodies in human lung tissue following death, embalmment, and burial.

The identification of asbestos bodies in tissue sections is an indicator of past exposure to longer asbestos fibers. These structures are formed in lung tissue as a consequence of interactions with pulmonary macrophages resulting in the deposition of a ferroprotein (ferruginous) coating on the fiber. While the process of ferruginous body formation is known to take months in animal tissue, there is no published information on the stability of ferruginous bodies in tissue following death. The material assessed in the present study was obtained from lung material collected from an exhumed body approximately 8(1/2) mo after death, embalmment, and burial. Tissue sections were reviewed for the presence of asbestos bodies. Additional pieces of lung tissue were digested, with the digestate being evaluated by light microscopy for ferruginous bodies and by electron microscopy for uncoated asbestos fibers and core analysis of asbestos bodies. Classical ferruginous (asbestos) bodies were found in abundance in the tissue sections including in areas with fibrosis. The levels of uncoated asbestos fibers and classical appearing ferruginous bodies (asbestos bodies) were consistent with occupational levels of tissue burden. The data from this study indicate that ferruginous bodies remain morphologically stable within the tissue for months following death, embalmment, and burial. Thus the lung tissue from this exhumed individual was usable not only to pathologically confirm asbestosis but also to provide quantitative data of occupational exposure to asbestos.

Aged, 80 and over↗

PubMed2003

Polar poisons: did Botulism doom the Franklin expedition?

In 1845 the Franklin expedition left London with 2 ships and 134 men on board in an attempt to find the route through the Northwest Passage. The ships were built with state-of-the-art technology for their day, but provisioned with supplies from the lowest bidder. After taking on fresh provisions in the Whalefish Islands, off the coast of Greenland, the entire crew was never heard from again. Graves found on remote Beechey Island indicate that three able-bodied seamen died during the first winter. A note written on a ship's log, later found in a cairn, indicate that the expedition's leader, Sir John Franklin, died during the second winter entrapped on the ice, by which time 24 men had also perished. The remaining crew failed in their attempt to walk out of the Arctic by an overland route. In 1981 Owen Beattie, from the University of Alberta, exhumed the remains of the sailors from the three graves on Beechey Island. Elevated lead levels were found in all three sailors. While lead poisoning has been a leading theory of the cause of the crew's deaths, blamed on the crudely tinned provisions the ships carried with them from England, chronic lead exposure may only have weakened the crew, not necessarily killed them. One of three exhumed sailors also had in his intestine the spores of an unspecified Clostridium species. The theory put forth by this article is that Botulism, type E, which is endemic in the Arctic, may have been responsible for their deaths.

Botulism↗

PubMed2000

Evidence for Differential Unroofing in the Adirondack Mountains, New York State, Determined by Apatite Fission-Track Thermochronology.

Apatite fission-track ages of 168-83 Ma for 39 samples of Proterozoic crystalline rocks, three samples of Cambrian Potsdam sandstone, and one Cretaceous lamprophyre dike from the Adirondack Mountains in New York State indicate that unroofing in this region occurred from Late Jurassic through Early Cretaceous. Samples from the High Peaks section of the Adirondack massif yielded the oldest apatite fission-track ages (168-135 Ma), indicating that it was exhumed first. Unroofing along the northern, northwestern, and southwestern margins of the Adirondacks began slightly later, as shown by younger apatite fission-track ages (146-114 Ma) determined for these rocks. This delay in exhumation may have resulted from burial of the peripheral regions by sediment shed from the High Peaks. Apatite fission-track ages for samples from the southeastern Adirondacks are distinctly younger (112-83 Ma) than those determined for the rest of the Adirondack region. These younger apatite fission-track ages are from a section of the Adirondacks dissected by shear zones and post-Ordovician north-northeast-trending normal faults. Differential unroofing may have been accommodated by reactivation of the faults in a reverse sense of motion with maximum compressive stress, sigma1, oriented west-northwest. A change in the orientation of the post-Early Cretaceous paleostress field is supported by a change in the trend of Cretaceous lamprophyre dikes from east-west to west-northwest.

Journal Article↗

PubMed2002

The body buried twice.

The authors report the case of an unusual reason for an "exhumation." A young person "exhumed" a child's body involved in a road accident because he wanted to test methods for preventing or slowing down the process of postmortem decay.

Female↗

PubMed2003

The case of Dr. Shipman.

On January 31, 2000, Dr. Harold Shipman was convicted at Preston, England, of murdering 15 of his patients by administering lethal doses of diamorphine (pharmaceutical heroin). Investigations indicate that, during his working life, he killed about 220 to 240 of his patients. The bodies of many victims were cremated. Twelve victims were exhumed, and 9 of these deaths were included in the indictment. Most victims were elderly and had histories of natural disease. Autopsies confirmed known natural disease but showed no evidence of acute lethal events. Analysis of skeletal muscle disclosed significant quantities of morphine, to which the deaths were attributed. Circumstantial evidence was strong, as illustrated by the convictions in 6 deaths without autopsy or toxicology, because the bodies had been cremated. Organic compounds are remarkably stable in buried bodies. Even so, detection and quantitation of morphine in exhumed bodies may become problematic after burial for 4 years or more. Morphine glucuronide is slowly converted back to free morphine in the buried corpse.

Aged↗

PubMed2006

Natural and experimental evidence of melt lubrication of faults during earthquakes.

Melt produced by friction during earthquakes may act either as a coseismic fault lubricant or as a viscous brake. Here we estimate the dynamic shear resistance (tau(f)) in the presence of friction-induced melts from both exhumed faults and high-velocity (1.28 meters per second) frictional experiments. Exhumed faults within granitoids (tonalites) indicate low tau(f) at 10 kilometers in depth. Friction experiments on tonalite samples show that tau(f) depends weakly on normal stress. Extrapolation of experimental data yields tau(f) values consistent with the field estimates and well below the Byerlee strength. We conclude that friction-induced melts can lubricate faults at intermediate crustal depths.

Journal Article↗

PubMed1990

Articulated cadaveric bones as a structural endoskeleton in an ankle-foot prosthesis: a preliminary report.

This report describes the construction and evaluation of an ankle-foot prosthesis using human cadaveric bones as the endoskeleton inside a fiber-reinforced vulcanized rubber shell. Cadaveric bones and exhumed skeletal bones were used. Three designs were fabricated, subjected to radiographic evaluation, and underwent 4-week field trials of normal daily use by a unilateral below-knee amputee. The rubber shell retained the position of the bones, permitted movements at the joints in various stages of the stance phase, and restored the bones to their neutral position when the foot was unloaded. The cadaveric prosthesis provided for plantar flexion of the foot when the heel was loaded and for locking of the joints to restrain excessive movement when the foot came to rest. While fresh cadaveric bones withstood all the stresses of active walking, exhumed macerated bones fractured and fragmented with use.

Ankle↗

PubMed2001

Mitochondrial DNA analysis of the presumptive remains of Jesse James.

We report here the results of mtDNA analysis of remains exhumed in July, 1995 from Mt. Olivet Cemetery in Kearney, Nebraska, that are thought to be those of Jesse James. The remains were poorly preserved, presumably due to wet and slightly acidic soil conditions, and insufficient DNA for analysis was obtained from two bone samples. However, two of four teeth, and two hairs recovered in 1978 from the original burial site on the James Farm, did yield reproducible mtDNA sequences. These mtDNA sequences from the teeth and hairs were all identical, suggesting that they came from the same individual; furthermore, this mtDNA sequence was identical to mtDNA sequences determined from blood samples from two maternal relatives of Jesse James. Therefore, either the remains are indeed those of Jesse James, or they are from an unrelated individual who, by chance, happens to have the same mtDNA sequence. To assess the probability that an unrelated individual would have the same sequence, we searched the forensic mtDNA database, and found that this sequence does not appear among the 2426 mtDNA sequences therein. Hence, the mtDNA analysis supports the identification of the exhumed remains from Mt. Olivet Cemetery as those of Jesse James.

Crime↗

PubMed2004

Factors affecting postmortem tooth loss.

Unassociated human bones are a particular problem during the exhumation of mass graves and a factor that limits anthropological and paleopathological analyses from archaeological contexts. Extensive anthropological literature has focused on the complex taphonomic factors that influences bone assemblages, but little attention has been paid to postmortem tooth loss and factors affecting this process. The following study focuses upon the influence of different factors on postmortem tooth loss. Three samples were investigated in the study: a medieval church cemetery containing 110 individual skeletal remains, and two samples from a series of mass graves made within the same time period in 1999, containing 402 bodies. The frequency of postmortem tooth loss was analyzed relative to postmortem interval for each sample, excavation methods, age distribution, and presence of bone loss associated with periodontal disease. Our results indicate that the degree of alveolar bone loss significantly affected both antemortem and postmortem tooth loss and that the frequency of postmortem tooth loss has the strongest correlation to time since death. These findings suggest that additional care should be taken when exhuming remains from older contexts.

Adolescent↗

PubMed1987

Identification of the cadaver remains of Josef Mengele.

In 1985 at the cemetery in Embu near Sao Paulo, Brazil, parts of a skeleton were exhumed, and now these parts have been examined to determine whether they are the remains of the corpse of Dr. Josef Mengele, the camp doctor of the Auschwitz concentration camp. The osteometrical and osteological findings ascertained correspond completely and consistently without contradiction with all the available personal data of Josef Mengele. Through a method of electronic visual mixing for the identification of the skull, it was determined that all the authentic pictures available used for comparison correspond definitely and consistently to the exhumed skull.

Aged↗

PubMedDate not supplied

[Identification of the cadaveric remains of Josef Mengele].

In 1985 at the cemetery in Embu near Sao Paulo, Brazil, parts of a skeleton were exhumed, and now these parts have been examined in order to determine whether they are the remains of the corpse of Dr. Josef Mengele, the camp doctor of the Auschwitz Concentration Camp. The osteometrical and osteological findings ascertained correspond completely and consistently without contradiction with all the available personal data of Josef Mengele. Through a method of electronic visual mixing for the identification of the skull, it was determined that all the authentic pictures available used for comparison correspond definitely and consistently in all details to the exhumed skull.

Forensic Medicine↗

PubMedDate not supplied

Radiographic evaluation of the soap man mummy.

This article describes how mobile radiography was used to examine a mummified cadaver exhumed in 1875 and stored in the Smithsonian Museum. Radiographs revealed artifacts imbedded in the cadaver, indicating 1824 as the earliest possible interment. Through radiographic assessment of the skeleton, researchers were able to approximate the individual's age at death. In addition, evidence of pathology, possibly ideopathic skeletal hyperostosis, suggested the individual may have been employed in manual labor. The radiographs, when compared to x-rays of another cadaver exhumed at the same time and place, refuted information in museum records.

Adipose Tissue↗

PubMed2005

Turf wars: authority and responsibility for the investigation of mass graves.

Mass graves are complex products of large-scale crimes. Such scenes pose four conceptual challenges to investigators and forensic experts: the individual victim, the crime, the setting, and the statistical. Exhumation and post-mortem examination of mortal remains with associated personal and forensic evidence require integrated management of core forensic personnel including investigators, archaeologists, anthropologists, odontologists and pathologists, among whom there is overlapping expertise. The key to avoiding competition and ill-will among experts is to recognize that all such experts should be enabled to make known how their expertise matches with the temporal and spatial boundaries of victim, crime and setting. In turn, they should be apprised of where they fit into the overall judicial process and their limits within the investigation. Consequently, each expert requires access to the factual background of the case, to the site and its contents throughout the investigation. Each forensic team member has a responsibility to influence the investigation--throughout its course when possible--to make findings within their areas of expertise, and to make these available to the rest of the team so as to contribute most meaningfully to the aims of the investigation, both forensic and humanitarian. The on-site crime scene manager has an overarching role to enable integrated access to the complete scene and its contents by each forensic expert team member. In other words, the forensic scientist is given access and the ability to influence the investigation while control of evidence from the site as to identity and criminal activity are maintained by the crime scene manager. This contribution is directed at both the crime scene manager and each forensic expert; it describes the essential spatial and temporal parameters of an expert's opinion so as to encourage cooperation, and discourage conflict, within the forensic team.

Burial↗

PubMed2005

The identification of mivacurium and metabolites in biological samples.

Mivacurium is a muscle relaxant that is used in hospitals and has been implicated in a number of homicides. A validated, sensitive method for the analysis of mivacurium and metabolites from biological specimens is presented here. Sample cleanup involves the precipitation of proteins with acetonitrile followed by analyte isolation using a commercially available solid-phase extraction column. Screening is performed by liquid chromatography with fluorescence detection, and confirmation is performed by liquid chromatography with tandem mass spectrometric detection. This method has been used to analyze dozens of forensic samples, including clinical specimens from living patients, as well as autopsy specimens from exhumed bodies.

Body Fluids↗

PubMed2005

The application of pancuronium bromide (Pavulon) forensic analyses to tissue samples from an "Angel of Death" investigation.

The case report of a serial killer who worked at several hospitals as a respiratory therapist is presented. The suspect was initially labeled a benevolent Angel of Death who ended the suffering of elderly patients through mercy killing. However, his subsequently declared motive for homicide was very different from other similar cases in medical settings. The application of new analysis techniques for the detection of pancuronium bromide in a series of aged exhumation tissues gave positive results and led to the resultant conviction of the therapist.

Adult↗

PubMedDate not supplied

[Cremation plant planning and related hygienic-sanitary aspects].

The number of cremators is set to grow in Italy owing to current increasing demand for cremation, as a system of burial as well as a system of disposal of non-decomposed human remains resulting from operations of exhumation (as provided by the Circular No. 10 of 31 July of 1998 of the Ministry of Health). Some indications on how town planners need to size up the cremation plant with regard to its capacity to face cremation demand, in order to avoid any hygienic-sanitary inconveniences are given. As a matter of fact, for planning the demand for cremation from Circular No. 10 of 31 July of 1998 it is necessary to assess the decomposition time in burial sites.

Exhumation↗