Pleistocene environments, climate, and human activity in Britain during Marine Isotope Stage 7: insights from Oak Tree Fields, Cerney Wick, Gloucestershire

Investigations at Oak Tree Fields, Cerney Wick, Gloucestershire, in western England have revealed a sequence of fluvial deposits dating from Marine Oxygen Isotope Stage (MIS) 7 to 5. At the base of the sequence, a series of gravel and sand facies were deposited, initially as part of a meandering river. Reductions in flow energy of the latter and avulsion led to the development of short-lived channels and episodic backwater environments, the deposits of which are recorded as Facies Associations 1–3. Poorly sorted, probably colluvial deposits formed beyond the limit of the channel (Facies Association 4). Mollusca, Coleoptera, plant macrofossils, pollen and vertebrates recovered from the channel facies indicate broadly similar climatic conditions throughout accretion. Temperature ranges derived from mutual climatic range analysis of the Coleoptera almost completely overlap with those of Cerney Wick at the present day, albeit that winters may have been cooler when the channel was active. Further, the floral and faunal data suggest that the meandering river flowed through an open grassland environment, the latter heavily grazed by large vertebrates, most notably mammoth. Most of the botanical and faunal remains, together with four optically stimulated luminescence (OSL) age estimates ranging from 225 ± 23 to 187 ± 19 ka, suggest correlation of the channel deposits with MIS 7. The basal deposits (Facies Association 1) yielded the majority of vertebrate remains and all the lithic artefacts, most of which seem likely to have travelled only a short distance. Although only a few artefacts were recovered, they add to the relatively limited evidence of human activity from the upper Thames. The channel deposits are overlain by sheet gravels (Facies Association 5) which are attributed to the Northmoor Member of the Upper Thames Formation. These were likely to have been deposited as bedload in a braided stream environment, while two OSL age estimates of 129 ± 14 and 112 ± 11 ka suggest accumulation during MIS 5

A concerted tryptophanyl-adenylate-dependent conformational change in bacillus subtilis tryptophanyl-tRNA synthetase revealed by the fluorescence of Trp92

A semi-conserved tryptophan residue of Bacillus subtilis tryptophanyl-tRNA synthetase (TrpRS) was previously asserted to be an essential residue and directly involved in tRNA(Trp) binding and recognition. The crystal structure of the Bacillus stearothermophilus TrpRS tryptophanyl-5'-adenylate complex (Trp-AMP) shows that the corresponding Trp91 is buried and in the dimer interface, contrary to the expectations of the earlier assertation. Here we examine the role of this semi-conserved tryptophan residue using fluorescence spectroscopy. B. subtilis TrpRS has a single tryptophan residue, Trp92. 4-Fluorotryptophan (4FW) is used as a non-fluorescent substrate analog, allowing characterization of Trp92 fluorescence in the 4-fluorotryptophanyl-5'-adenylate (4FW-AMP) TrpRS complex. Complexation causes the Trp92 fluorescence to become quenched by 70%. Titrations, forming this complex under irreversible conditions, show that this quenching is essentially complete after half of the sites are filled. This indicates that a substrate-dependent mechanism exists for the inter-subunit communication of conformational changes. Trp92 fluorescence is not efficiently quenched by small solutes in either the apo- or complexed form. From this we conclude that this tryptophan residue is not solvent exposed and that binding of the Trp92 to tRNA(Trp) is unlikely. Time-resolved fluorescence indicates conformational heterogeneity of B. subtilis Trp92 with the fluorescence decay being best described by three discrete exponential decay times. The decay-associated spectra (DAS) of the apo- and complexed-TrpRS show large variations of the concentration of individual fluorescence decay components. Based on recent correlations of these data with changes in the local secondary structure of the backbone containing the fluorescent tryptophan residue, we conclude that changes observed in Trp92 time-resolved fluorescence originate primarily from large perturbations of its local secondary structure. The quenching of Trp92 in the 4FW-AMP complex is best explained by the crystal structure conformation, in which the tryptophan residue is found in an α-helix. The amino acid residue cysteine is observed clearly within the quenching radius (3.6 Å) of the conserved tryptophan residue. These tryptophan and cysteine residues are neighbors, one helical turn apart. If this local α-helix was disrupted in the apo-TrpRS, this disruption would concomitantly relieve the putative cysteine quenching by separating the two residues. Hence we propose a substrate-dependent local helix-coil transition to explain both the observed time-resolved and steady-state fluorescence of Trp92. A mechanism can be further inferred for the inter-subunit communication involving the substrate ligand Asp132 and a small α-helix bridging the substrate tryptophan residue and the conserved tryptophan residue of the opposite subunit. This putative mechanism is also consistent with the observed pH dependence of TrpRS crystal growth and substrate binding. We observe that the mechanism of TrpRS has a dynamic component, and contend that conformational dynamics of aminoacyl-tRNA synthetases must be considered as part of the molecular basis for the recognition of cognate tRNA

Resumption of Cardiac Activity after Withdrawal of Life-Sustaining Measures

BACKGROUNDThe minimum duration of pulselessness required before organ donation after circulatory determination of death has not been well studied.METHODSWe conducted a prospective observational study of the incidence and timing of resumption of cardiac electrical and pulsatile activity in adults who died after planned withdrawal of life-sustaining measures in 20 intensive care units in three countries. Patients were intended to be monitored for 30 minutes after determination of death. Clinicians at the bedside reported resumption of cardiac activity prospectively. Continuous blood-pressure and electrocardiographic (ECG) wave-forms were recorded and reviewed retrospectively to confirm bedside observations and to determine whether there were additional instances of resumption of cardiac activity.RESULTSA total of 1999 patients were screened, and 631 were included in the study. Clinically reported resumption of cardiac activity, respiratory movement, or both that was confirmed by waveform analysis occurred in 5 patients (1%). Retrospective analysis of ECG and blood-pressure waveforms from 480 patients identified 67 instances (14%) with resumption of cardiac activity after a period of pulselessness, including the 5 reported by bedside clinicians. The longest duration after pulselessness before resumption of cardiac activity was 4 minutes 20 seconds. The last QRS complex coincided with the last arterial pulse in 19% of the patients.CONCLUSIONSAfter withdrawal of life-sustaining measures, transient resumption of at least one cycle of cardiac activity after pulselessness occurred in 14% of patients according to retrospective analysis of waveforms; only 1% of such resumptions were identified at the bedside. These events occurred within 4 minutes 20 seconds after a period of pulselessness. (Funded by the Canadian Institutes for Health Research and others.