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Abstract: The taxonomy and biostratigraphic significance of horses (Equus), deer (Capreolus, Dama, Cervus, Cervalces, Praemegaceros, Megaloceros) and pigs (Sus) from key British early Middle Pleistocene sites are investigated using a biometric approach. The sites compared are West Runton (type Cromerian), Pakefield, Little Oakley, Westbury-sub-Mendip, and Boxgrove. The samples include a significant amount of previously undescribed material. Stenonid horses dominate at Pakefield and West Runton, caballines at Westbury and Boxgrove, corresponding to the Mimomys/Arvicola division. The deer of Boxgrove include relatively large roe and small red deer, the latter distinguishing it from the Westbury Pink Breccia. The poorly-known giant deer Praemegaceros dawkinsi spans both the Mimomys (Little Oakley, Pakefield) and Arvicola (Boxgrove) zones of the Cromerian Complex. There is a marked shift in cervid abundance from predominant megacerines (Mimomys zone) to predominant red deer (Arvicola zone). [ABSTRACT FROM AUTHOR]

Abstract: In 1995–1996 two isolated hominin lower incisors were found at the middle Pleistocene site of Boxgrove in England, with Lower Palaeolithic archaeology. Boxgrove 2 is a permanent lower right central incisor and Boxgrove 3 a permanent lower left lateral incisor. They were found separately, but close to one another and appear to belong to the same individual. The Boxgrove 1 tibia discovered in 1993 came from a different stratigraphic context and is thus believed to represent a different individual. This paper describes the morphology of the incisors, which is similar to other middle Pleistocene hominin specimens and, as with the tibia, suggests that they could be assigned to Homo heidelbergensis (recognising that the taxonomic status of this species is still a matter of debate). The incisors show substantial attrition associated with secondary dentine deposition in the pulp chamber and clearly represent an adult. They also show extensive patterns of non-masticatory scratches on the labial surfaces of both crown and root, including some marks which may have been made postmortem. The roots were exposed in life on their labial sides by a large dehiscence, extending almost to the root apex. This is demonstrated by deposits of calculus, polishing, and scratching on the exposed surfaces. The dehiscence may have been caused by repeated trauma to the gingivae or remodelling of the tooth-supporting tissues in response to large forces applied to the front of the dentition. [ABSTRACT FROM AUTHOR]

Abstract: Multidisciplinary investigations of the sequence at Beeches Pit, West Stow (Suffolk, UK), have a direct bearing the age of the Hoxnian Interglacial and its correlation with the continental Holsteinian and with the global marine record. At this site, glacial deposits (till and outwash gravels) referable to the Anglian Lowestoft Formation fill a subglacial channel cut in Chalk bedrock. Above these glacial deposits a series of interglacial sediments occurs, consisting of limnic, tufaceous and colluvial silts, lacking pollen but rich in shells, ostracods and vertebrates. Lower Palaeolithic flint artefacts of Acheulian character have also been recovered, including refitting examples. Charred material is abundant at certain horizons and many of the bones have been burned. Several discrete areas of burnt sediment are interpreted as hearths. The molluscan fauna comprises some 78 taxa and includes species of considerable zoogeographical and biostratigraphical importance. The land snail assemblage from the tufa consists of woodland taxa with no modern analogue, including species that are either extinct (e.g. Zonitoides sepultus) or which no longer live in Britain (e.g. Platyla polita, P. similis, Neniatlanta pauli). This is also the type locality of Retinella (Lyrodiscus) skertchlyi, which belongs to a subgenus of zonitid land snail now living only on the Canary Islands. There are indications from this fauna (‘the Lyrodiscus biome’) that the climate was wetter and perhaps warmer than the present day. The vertebrate fauna is also noteworthy with species of open habitats, such as rabbit (Oryctolagus cf. cuniculus), and of closed forest, such as squirrel (Sciurus sp.) and garden dormouse (Eliomys quercinus) present at different times. The occurrence of southern thermophiles, such as Aesculapian snake (Zamenis longissimus), indicates temperatures warmer than those of eastern England today. The upper levels include much material reworked from the interglacial sediments, although there is clear faunal evidence for climatic deterioration. Both the molluscan and vertebrate faunas suggest correlation of the interglacial sediments with the Hoxnian. Uranium series dates from the tufa (∼455ka BP), TL dates from burnt flints (414±30ka BP) and a range of amino acid racemization data all support correlation of this interglacial with MIS 11. However, four OSL dates from sand beneath the interglacial sequence yield a mean age of 261±31kaBP, far younger than all other age determinations and far younger than implied by the biostratigraphy. Archaeologically the site is unusual in showing prolonged human occupation within closed deciduous forest and evidence for controlled use of fire in a Lower Palaeolithic context. Biostratigraphical correlations with other Lower Palaeolithic sites support the suggestion that Acheulian and Clactonian industries both occurred in southern Britain during the same substage of the Hoxnian, although not necessarily at precisely the same time. The characteristics of the MIS 11 interglacial in Britain are discussed in the light of evidence from Beeches Pit and elsewhere. [Copyright &y& Elsevier]

Abstract: Rhinoceroses (Stephanorhinus) and large bovids (Bison, Bos) from the early Middle Pleistocene of Britain are analysed with regard to their taxonomy, biometric variation, and possible biochronological significance. The localities considered are West Runton (type Cromerian), Pakefield, Westbury-sub-Mendip, and Boxgrove. The samples include important, previously undescribed material. Among the rhinos, in addition to the common Stephanorhinus hundsheimensis, upper dentitions from Pakefield and West Runton provide hints of undescribed taxa with affinity to, but distinct from, S. etruscus and S. hundsheimensis. At Boxgrove, a further rhino cf. S. megarhinus occurs, corroborating the chronological extension of this ‘Pliocene’ species into the Middle Pleistocene. A small bison referable to B. schoetensacki occurs at all sites, but in the Westbury Yellow Breccia (upper interglacial level) it is accompanied by a larger bison which may be B. priscus. Dental material from Pakefield provides evidence of additional, smaller bovid species, with features recalling Leptobos and Bubalus, but their identity is unclear; there is also larger material probably representing Bos, which if confirmed would be the oldest record of aurochs in the British Isles. [ABSTRACT FROM AUTHOR]

Abstract Ground squirrels were an important member of the Pleistocene steppe-tundra mammal community. They evolved ecological specialisations and exhibit behaviours that make them particularly informative subjects to study palaeoenvironmental constraints affecting species distribution and speciation. Interspecific competition and isolating geographical barriers are considered as the principal factors that define species range boundaries. The present paper provides a first comprehensive compilation of the living and extinct Spermophilus species in Europe. These data suggest 'patchwork quilt' model for the expansion and spatial distribution of ground squirrel species. Here we consider mainly small-sized Spermophilus species because large-sized (e.g., S. superciliosus) ground squirrels consist another 'patchwork quilt', which overlap the first one. This overlapping of the species ranges is possible because of the size difference that lowers interspecific competition (Hutchinson's rule). We consider two main types of range boundaries. One type includes roughly 'sub-parallel' boundaries that oscillate in concert with climatic and vegetational changes (a case of climatically controlled competitive exclusion). The other type consists of roughly 'sub-meridional' boundaries corresponding to geographical barriers (e.g., water barriers, mountain ridges); these boundaries are rather stable. Examples of 'sub-parallel range modifications include: oscillations of boundaries between S. pygmaeus and S. suslicus ; the immigration of S. citellus into the Pre-Carpathian area; the branching of S. suslicus from S. pygmaeus ; the regional appearance of the Late Pleistocene species S. severskensis and S. citelloides. Examples of 'sub-meridional events' are: the crossing of the Danube by S. citellus ; the appearance of an isolated population of S. pygmaeus on right bank of the Dnieper during the Late Pleistocene to Middle Holocene; a crossing of the Dnieper river by S. pygmaeus , which resulted in the appearance of S. odessanus ; the intrusion of eastern populations of S. pygmaeus into the Trans-Volga areas. [ABSTRACT FROM AUTHOR]

This paper presents evidence of the discovery of a new Middle Pleistocene site in central southern England, with undisturbed evidence of hominin occupation well-dated to an interstadial towards the end of Marine Isotope Stage 8, c. 250,000 BP. The site consists of a preserved remnant of a river terrace and its alluvial floodplain overlain by chalk-rich bankside deposits, all abutting a Chalk bedrock riverbank. It preserves an area of occupation with activity focused on the riverbank, complemented by occasional activity on a palaeo-landsurface developed on the surface of the alluvial floodplain. Lithic technology at the site consists almost entirely of handaxe manufacture, allowing attribution to an Acheulian industrial tradition. Mammalian and other palaeo-environmental remains are present and associated with the occupation horizons, including large mammal bones showing signs of hominin interference. Dating was based on OSL determinations on the sediments and amino acid racemisation of molluscan remains, supported by biostratigraphic indications. Besides being a rare instance of an undisturbed Palaeolithic palaeo-landscape covering several hectares, the site contributes to wider Quaternary research concerns over the ability of Middle Pleistocene hominins to tolerate colder climatic episodes in higher latitudes, and over settlement history and changing lithic industrial traditions of northwest Europe in relation to climate change and British peninsularity. It is suggested that the Harnham evidence may represent an insular population that had persisted in southern Britain since MIS 10/9, which became locally extinct during the glacial maximum 8.2 marking the end of MIS 8. [ABSTRACT FROM AUTHOR]

Abstract: The Mid-Brunhes Event (MBE) is a climatic transition occurring between MIS 13 and 11 that separates two climatic modes: (1) early Middle Pleistocene interglacials (780–450ka) that are characterised by only moderate warmth and (2) Middle and Late Pleistocene interglacials (occurring after 450ka) that are characterised by greater warmth consistent with, or warmer than, the Holocene. This event is observable within a variety of long climate records, such as SPECMAP and EPICA, but its effect on terrestrial systems is poorly understood. The impact of this event is examined in the British terrestrial sequence by comparing the occurrence of a range of thermophilous plant and animal species, and climate reconstructions derived from assemblages containing them, from interglacials of the early Middle Pleistocene with those from the late Middle and Late Pleistocene. This comparison reveals that interglacial climates during the early Middle Pleistocene in Britain were as warm as, and in some cases warmer than, those that occurred during the late Middle and Late Pleistocene. This interpretation is supported by sea surface temperature records in the North Atlantic, which show that temperatures during early Middle Pleistocene interglacials were at least as warm as those experienced during the Holocene. There is, therefore, no evidence in climate records of Britain and the North Atlantic for a Mid-Brunhes Event. This suggests that the MBE is not a global climatic transition but is restricted to specific regions, in particular the higher latitudes of the southern Hemisphere. Further work is needed to understand the regional variability and cause of the MBE. [ABSTRACT FROM AUTHOR]