New geochronological, paleoclimatological, and archaeological data from the Narmada Valley hominin locality, central India.

The oldest known fossil hominin in southern Asia was recovered from Hathnora in the Narmada Basin, central India in the early 1980's. Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at >236ka, but not likely older than the early middle Pleistocene. The calvaria, however, could be considerably younger. We report recent fieldwork at Hathnora and associated Quaternary type-sections that has provided new geological and archaeological insights. The portion of the exposed 'Boulder Conglomerate' within the Surajkund Formation, which forms a relict terrace and has yielded the hominin fossils, contains reworked and stylistically mixed lithic artifacts and temporally mixed fauna. Three mammalian teeth stratigraphically associated with the hominin calvaria were dated by standard electron spin resonance (ESR). Assuming an early uranium uptake (EU) model for the teeth, two samples collected from the reworked surface deposit averaged 49+/-1ka (83+/-2ka, assuming linear uptake [LU]; 196+/-7ka assuming recent uptake [RU]). Another sample recovered from freshly exposed, crossbedded gravels averaged 93+/-5ka (EU), 162+/-8ka (LU) or 407+/-21ka (RU). While linear uptake models usually provide the most accurate ages for this environment and time range, the EU ages represent the minimum possible age for fossils in the deposit. Regardless, the fossils are clearly reworked and temporally mixed. Therefore, the current data constrains the minimum possible age for the calvaria to 49+/-1ka, although it could have been reworked and deposited into the Hathnora deposit any time after 160ka (given the LU uptake ages) or earlier (given the RU ages). At Hathnora, carbonaceous clay, bivalve shells, and a bovid tooth recovered from layers belonging to the overlying Baneta Formation have yielded (14)C ages of 35.66+/-2.54cal ky BP, 24.28+/-0.39cal ky BP, and 13.15+/-0.34ky BP, respectively. Additional surveys yielded numerous lithics and fossils on the surface and within the stratigraphic sequence. At the foot of the Vindhyan Hills 2km from the river, we recovered a typologically Early Acheulean assemblage comprised of asymmetrical bifaces, large cleavers with minimal working, trihedral picks, and flake tools in fresh condition. These tools may be the oldest Acheulean in the Narmada Valley. Several lithics recovered from the Dhansi Formation may represent the first unequivocal evidence for an early Pleistocene hominin presence in India. In situ invertebrate and vertebrate fossils, pollen, and spores indicate a warm, humid climate during the late middle Pleistocene. High uranium concentrations in the mammalian teeth indicate exposure to saline water, suggesting highly evaporative conditions in the past. Late Pleistocene sediment dated between 24.28+/-0.39cal ky BP and 13.15+/-340ky BP has yielded pollen and spores indicating cool, dry climatic conditions corresponding to Oxygen Isotope Stage 2 (OIS 2). An early Holocene palynological assemblage from the type locality at Baneta shows evidence for relatively dry conditions and a deciduous forest within the region. The Dhansi Formation provisionally replaces the Pilikarar Formation as the oldest Quaternary formation within the central Narmada Basin. The Baneta Formation, previously dated at 70ka to 128ka, correlates with the late Pleistocene and early Holocene. Our results highlight the need for further Quaternary geological and paleoanthropological research within the Narmada Basin, especially because dam construction threatens these deposits.

ESR dating at Mezmaiskaya Cave, Russia.

Mezmaiskaya Cave has yielded more than 10,000 artifacts, thousands of very well preserved faunal remains, and hominin remains, found in seven Middle Paleolithic (Mousterian) and three Upper Paleolithic levels. A complete Neanderthal infant skeleton was preserved in anatomical juxtaposition lying on a large limestone block, overlain by the earliest Mousterian layer, Layer 3. Twenty-four skull fragments from a 1-2 year-old Neanderthal infant, showing post-mortem deformation, occurred in a pit originating in the Mousterian Layer 2 and penetrating into underlying layers 2A and 2B(1). Bone from Layer 2A was dated by AMS 14C at 35.8-36.3+/-0.5 kyr BP. Direct dating of Neanderthal bone from Layer 3 gave an age of 29 kyr, but that is now considered to be due to contamination by modern carbon. Fourteen large mammal teeth from Layers 2 through 3 have been dated by standard electron spin resonance (ESR). Low U concentrations in both the enamel and dentine ensure that ESR ages do not depend significantly on the U uptake model, but do depend strongly on the sedimentary dose rates. Assuming a sedimentary water concentration equal to 20 wt%, ESR ages for the Mousterian layers range from 36.2 to 73.0+/-5.0 ka.

Analysis of Fusarium graminearum mycotoxins in different biological matrices by LC/MS.

The purpose of this study was to develop an LC/MS assay to accurately detect three mycotoxins produced by Fusarium graminearum in various matrices. Using different LC conditions, deoxynivalenol (DON), 15-acetyldeoxynivalenol (15-ADON), and zearalenone (ZEN) were detected in four different matrices (fungal liquid cultures, maize grain, insect larvae and pig serum). The sensitivity of MS detection allowed us to detect concentrations as low as 8 ppb of DON and 12 ppb of ZEN. A very small quantity of matrix was therefore necessary for successful analysis of these toxins and a variety of experimental situations were successfully investigated using this technique. Production of 15-ADON and butenolide was monitored in a liquid culture of F. graminearum under controlled conditions. Using simple extraction procedures, the differential accumulation of DON and 15-ADON was followed in inoculated maize genotypes varying in susceptibility to F. graminearum. Toxicokinetic studies were carried out with maize insect pests reared continually on artificial diets containing ZEN and suggested that larvae may possess the ability to degrade ZEN. Finally, persistence of DON was assessed in pigs fed diet supplemented with DON, results indicated that DON accumulates quickly in pig blood and then levels decline progressively for 12 hours thereafter. The LC/MS study reported here is very useful and flexible for the detection of these mycotoxins in different media and at very low concentrations.

A new 1-hydroxy-2,6-pyrazinedione associated with hypovirulent isolates of Sclerotinia minor.

A new 1-hydroxy-2,6-pyrazinedione, sclerominol (1), was isolated from cultures of hypovirulent isolates of Sclerotinia minor, a fungal plant pathogen associated with lettuce drop and other plant diseases. This compound was characterized by NMR, mass spectrometry, and X-ray crystallography. One other 1-hydroxy-2,6-pyrazinedione, flutimide, has been reported. Flutimide has activity as an inhibitor of influenza virus endonuclease, and therefore, sclerominol was evaluated for related biological activity. Sclerominol (1) displayed some activity against cancer cell lines but little activity against three influenza virus strains. The role of 1 in the physiology of hypovirulent isolates of S. minor has not been determined, but 1 has also been recovered from debilitated isolates of S. sclerotiorum.

Improvements in dating tooth enamel by ESR.

ESR dating requires that growth curves be determined by interpreting complex spectra. Spectra, however, can vary significantly in shape and field position between different samples, or occasionally between subsamples, even though the mineralogy remains the same. In some cases, this spectral variability does not affect the resulting accumulated dose calculation. In other cases, signal subtraction may be needed. However, some samples that until recently might have been considered unsuitable for dating are now shown to yield accurate and precise results because a broad interference peak is integral to the hydroxyapatite signal. By studying the spectrum at the Q-band frequency, it can be shown that the interfering signal in most cases is not a problem for dating. A second concern has been that artificially irradiating sample aliquots can introduce a short-lived component that is simply an unstable enhancement of the dating signal. The apparent accumulated dose from growth curves created immediately after irradiation is considerably greater than that after annealing, although the curve's shape remains unchanged. Annealing both the natural and artificially irradiated signal shows the dating signal's lifetime to be greater than 10(10) years.

Oxidative deamination of hydrolyzed fumonisin B(1) (AP(1)) by cultures of Exophiala spinifera.

Fumonisins are mycotoxins of world-wide distribution in maize infected by the fungus Fusarium verticillioides. They are highly toxic to certain livestock and are potential carcinogens. Exophiala spinifera, a black yeast fungus found on moldy maize kernels, was identified previously as capable of growing on fumonisin B1 as a sole carbon source and thus is a potential source for fumonisin detoxifying enzymes. Pure cultures of E. spinifera transform fumonisin B(1) to the amino polyol AP(1) plus free tricarballylic acid through the activity of a soluble extracellular esterase, and further transformation is evidenced by accumulation in culture supernatant of a less polar compound(s) lacking a fluorescamine-reactive amino group. A free amine is thought to be critical for biological activity of FB(1) or AP(1). As a first step towards characterizing this amine-modifying activity, we investigated the biotransformation of AP(1) by E. spinifera liquid cultures that had been previously grown in liquid medium containing AP(1) as a sole carbon source. Accumulation of AP(1)-derived metabolites was monitored by thin-layer chromatography of culture supernatants, and product metabolites were purified and evaluated by mass spectrometry and nuclear magnetic resonance. Two products of treatment of purified AP(1) with cultures of E. spinifera are shown to be N-acetyl AP(1) and a new compound, 2-oxo-12,16-dimethyl-3,5,10, 14,15-icosanepentol hemiketal (or 2-OP(1) hemiketal).

Identification of a new sphingolipid 3-O-acyl-D-erythro-sphingomyelin in newborn pig and infant plasma.

A new sphingolipid was found in newborn pig plasma at a level of 2.5 +/- 0.4% of total lipids. The compound decreased to less than half that amount by day one of age and virtually disappeared by the fourth week. On thin-layer chromatography (TLC) the new lipid migrated close to phosphatidylethanolamine. The compound was isolated by TLC from the plasma of newborn piglets and identified as a 3-O-acyl-D-erythro-sphingomyelin by chemical and chromatographic techniques, 1H- and 13C-nuclear magnetic resonance and fast-atom bombardment mass spectrometry. Mild alkaline hydrolysis at room temperature gave mainly C16 and C18 fatty acids and sphingomyelin. Subsequent reaction with Ba(OH)2 released long-chain saturated and monounsaturated fatty acids from C14 to C24, and sphingosine which was identified as the erythro configuration by gas chromatography. Less than 1% of the sphingosine was of the C20 isomer. No hydroxy fatty acids were found. The acylated sphingomyelin was only found in plasma lipids of newborn piglets and not in their red blood cell membranes or platelets of newborn piglets, or in sow plasma. This compound was tentatively identified by chromatography in trace amounts in the serum of cord blood of newborn infants, but not in the plasma lipids of adults.

NMR structural studies of fumonisin B1 and related compounds from Fusarium moniliforme.

Fumonisin B1 (FB1) is the primary mycotoxin produced by Fusarium moniliforme and appears to be responsible for the varied toxigenic effects associated with ingestion of this mold, particularly that of the inhibition of sphingolipid biosynthesis. Understanding the structure and biosynthesis of fumonisins is a key factor in determining structure/activity relationships. To this end, Nuclear Magnetic Resonance (NMR) methods have been used to identify various derivatives of FB1, both naturally occurring and synthetic. With accurate chemical shift assignments, NMR may be used to determine the level of impurities in toxicological grade FB1 preparations. Specifically enriched FB1 was prepared from F. moniliforme cultures using 13C-enriched acetate as well as several 13C-enriched amino acids. 13C NMR analysis indicates that the biosynthesis of fumonisins involves the addition of methionine-derived methyl functions, glutamate-derived tricarballylic ester functions and alanine to an 18 carbon hydrocarbon backbone that is likely polyketide in origin. With the goal of obtaining a crystalline compound for the determination of absolute configuration, several derivatives of FB1 have been prepared, and NMR analysis used to determine the relative and absolute configuration of the 10 stereocenters present in this molecule.

Isolation and characterization of new chlamydosporol related metabolites of Fusarium chlamydosporum and Fusarium tricinctum.

Fusarium chlamydosporum strain T-826 isolated from corn in the USA produced chlamydosporol and two analogs which have been identified by various spectroscopic techniques as: 7,8-dihydro-5-hydroxy-4-methoxy-trans-7,8-dimethyl-2H,5H-pyrano(4, 3-b)pyran-2-one (or isochlamydosporol) and 4-methoxy-5-hydroxymethyl-6-(3-butan-2-ol)-2H-pyran-2-one (or chlamydospordiol). Chlamydosporol (compound a + b) chlamydospordiol (compound c) and isochlamydosporol (compound d) were produced together (up to 6000 micrograms/g) by 3 out of 11 isolates of F. chlamydosporum and by 3 out of 24 isolates of F. tricinctum from various substrates and geographic origin. Three isolates of F. chlamydosporum and one isolate of F. tricinctum produced only chlamydospordiol and 2 isolates of F. tricinctum produced chlamydosporol (a + b), and chlamydospordiol (c).

Ion transport and methane production in Methanobacterium thermoautotrophicum.

In Methanobacterium thermoautotrophicum, the protonmotive force for the H+-translocating ATPase consists mainly of a transmembrane electrical gradient (Deltapsi). These cells do not establish a significant transmembrane pH gradient (inside alkaline) and, in fact, if the suspending medium is of pH >/= 7.0, the pH gradient may be reversed-i.e., inside acid with respect to the extracellular pH. These studies show by both 23Na NMR and 22Na+ distribution that Na+ extrusion with the generation of Deltapsi precedes methanogenesis in Mb. thermoautotrophicum. It is calculated that the newly established Na+ gradients increase Deltapsi by approximately 50 mV (inside negative). There is no detectable H+ extrusion during methane synthesis; instead there is a high rate of H+ consumption for methane synthesis and an increase in internal pH. This was supported by 31P NMR experiments, which showed an internal pH shift from 6.8 to 7.6. With the cells maintained at an external pH of 7.2, the initial transmembrane pH gradient of -0.4 (inside acid) at 60 degrees C is equivalent to Deltapsi of + 27 mV (inside positive); after 20 min of incubation, the transmembrane pH gradient is + 0.4 (inside alkaline), which at 60 degrees C is equivalent to Deltapsi of -27 mV (inside negative). Actively respiring cells generated a protonmotive force of -198 mV. It is proposed that energy for CO2 reduction to the level of formaldehyde (the first step in methane synthesis) in Mb. thermoautotrophicum is derived from the Deltapsi generated by electrogenic Na+ extrusion. The protonmotive force required for ATP synthesis consists primarily of Deltapsi and appears to be the result of both an electrogenic Na+ extrusion and a pH gradient (inside alkaline) which develops during methanogenesis.