Dwellings and workspaces at Strandvägen, 5600–5000 cal. BC

This paper describes identified workspaces and the manufacture of slotted bone points at the Late Mesolithic settlement Strandvägen in Motala, in eastern central Sweden. Several dwellings were documented, Dwelling 1 being typically round-oval in shape 9 × 5.5 meters, with a floor area covering 49.5 m². Radiocarbon dates fall between approximately 5600-5200 cal BC. A combined archaeological record, with lithics and bone artefacts as well as analyses of the osteological assemblage has shown that slotted bone tools with mounted lithic inserts have been produced adjacent of the dwelling. The spatial distribution of bone flakes, microblades, processed resin and slotted artefacts testify to a clearly and delimited craft area near the shoreline of the river Motala Ström. Analyses of the finds, e.g. birch bark resin and prepared bone preforms by direct percussion, also help in reconstructing the stages of manufacturing composite projectile points in this part of Eurasia.     

The open-air Paleolithic site of Mirak,northern edge of the Iranian Central Desert (Semnan,Iran): Evidence of repeated human occupations during the late Pleistocene

The northern edge of the Iranian Central Desert has provided valuable evidence of terminal Pleistocene human settlements. Mirak constitutes one of the largest open-air lithic scatters in the region, consisting of eight natural mounds. Fieldwork was initiated in 2015 by the joint Iranian-French program at Mirak 8. Preliminary results have demonstrated at least three successive phases of human occupation during the MIS3: an upper layer with clear Upper Paleolithic affinities and a maximum age of 28 ky, a lower layer with clear Middle Paleolithic affinities that dates around 47 ky, and an intermediate layer with mixed characteristics that can be seen as an intermediate Paleolithic phase which dates between 28 ± 2 and 38 ± 2 ky. At the time when Upper Paleolithic cultures originated in the Zagros Mountains, cultures with clear Middle Paleolithic affinities persisted nearby along the northern edge of the Iranian Central Plateau.     

Late Pleistocene to Middle Holocene lithic industries from Southernmost Patagonia. Discussing technical variability,continuity and innovations

The study of early lithic assemblages from South America's Southern Cone used to be strongly focused on projectile points, including the famed fishtail type, often using a typological approach. The last three decades have seen a growing diversification of theoretical and methodological approaches to lithic studies, as well as new analytical techniques, used to study issues including lithic production systems, technical variability, tool manufacturing and management, raw material economy and circulation, among others. Recent studies on lithic industries are exemplified by discussing Southernmost Patagonia's first human occupations, dated ∼13,000 cal BP, and Middle Holocene early marine explorations, dated ∼8000–7000 cal BP. An overview and comparison of Southernmost Patagonia's early hunter-gatherer lithic technologies is made.     

New data on the Late Mousterian in Mediterranean France: First radiocarbon (AMS) dates at Saint-Marcel Cave (Ardèche)

This article presents new accelerator mass spectrometry (AMS) radiocarbon dates of cutmarked ungulate remains from one of the uppermost archaeological layers (f) at the Grotte de Saint-Marcel, Ardèche, France. This site is situated in a key location regarding population dispersal and potential interaction between Neanderthals and modern humans, as it lies at the crossroads of two main routes of passage. Attributing the upper sequence of this site to a precise chronological period within the Mousterian was difficult until now. Previous conventional ¹⁴C analyses done on bulk samples over twenty years ago were considered too young (23,000–30,000 BP). Our new AMS radiocarbon results give two statistically identical dates of 37,850 ± 550 BP and 37,850 ± 600 BP, thus confirming the Late Mousterian attribution of the upper levels of this site. A third date overlaps them at two standard deviations. These are among the very few chronometric dates available for the Mousterian (especially its late phases) in Mediterranean France. The Late Mousterian of this zone, a key region in recent debates about late Neanderthal behaviour, is discussed in light of these results.     

Holocene environmental changes as recorded by mineral magnetism of sediments from Anguli-nuur Lake,southeastern Inner Mongolia Plateau,China

Two cores, one 1141-cm long (An-S) and the other 885-cm long (An-A), were retrieved from Anguli-nuur Lake (41°18′–24′N, 114°20′–27′E, ～ 1315 masl), one of the largest lakes in the transition zone between a semi-humid and semi-arid climate parallel to the present limit of the southeast monsoon along the southeastern Inner Mongolia Plateau in north China. Mineral-magnetic parameters (χ_lf, ARM, IRM_300mT, SIRM and IRM_? 300mT) were measured on An-S and two additional parameters (χ_ARM and HIRM) and four inter-parametric ratios (χ_ARM/SIRM, IRM_300mT/SIRM, IRM_? 300mT/SIRM and SIRM/χ_lf) were calculated. Potential sources of these lake sediments (catchment soils and dune materials close to the lake and in a distant sand plain) were sampled, and the magnetic properties of the surface-material specimens were measured. A chronological model was developed for An-S by comparing and combining AMS¹⁴C dates of An-S with ¹³⁷Cs, ²¹⁰Pb and AMS¹⁴C dates of An-A. With the help of surface-material magnetism, the magnetic data of An-S in combination with particle size, TOC and C/N and pollen analyses indicate the environmental changes during the last ～ 10,000 years around this lake. Conditions began to ameliorate at 10,900 cal. yr BP (9600 ¹⁴C yr BP) and thus relatively wet and warm environments prevailed during 10,900–8900 cal. yr BP (9600–8000 ¹⁴C yr BP). The Holocene optimum or the wettest and warmest conditions, was during 8900–7400 cal. yr BP (8000–6500 ¹⁴C yr BP). The environment began to deteriorate from 7400 cal. yr BP (6500 ¹⁴C yr BP) and the driest and coolest conditions occurred during 2200–480 cal. yr BP. There may have been a minor amelioration after 480 cal. yr BP. The inferred changes in palaeoenvironmental conditions around Anguli-nuur Lake are broadly in agreement with those around most other sites on the Inner Mongolia Plateau.     

Chasseurs épigravettiens dans le territoire de l’ours des cavernes : le cas du Covolo Fortificato di Trene (Vicenza,Italie)

The Covolo Fortificato di Trene site is located on the eastern slope of the Berici hills, Vicenza, in the middle of the great Po-venetian plain in Northern Italy, at a height of 360 m.a.s.l. The cavity was the object of systematic excavations made by the University of Ferrara in 1956, which yielded a 1.14 m-thick deposit, subdivided into seven stratigraphic units. The lithic industry, associated with macromammals remains, bird bones and charcoal, ascribe the anthropic frequentation of the archeological layers to the early Epigravettian. This is confirmed by two dates obtained on bone (17.640 ± 140 AMS ¹⁴C B.P. and 18.630 ± 150 AMS ¹⁴C B.P.). This work presents a taxonomic revision and zooarchaeological analysis of already published faunal remains, whose spectrum shows a clear dominance of Ursus spelaeus over the other determined taxa. During human frequentation, the site was in a predominantly forest environment under cold-temperate climate conditions with wetland areas on the underlying plain, as shown by the presence of elk, deer, wild boar and fish vertebrae. The taphonomic analysis has shown anthropic traces on the remains of elk and cave-bear, which used the cave as den during wintering. The study focused on Ursidae remains, affected by butchering marks due to fur extraction, mostly from young individuals. Moreover, a limited comparison (Berici hills) with contemporary sites (Paina cave, Buso Doppio cave), associates cave-bear presence with shouldered points.     

Nouvelles données sur le Magdalénien inférieur de la Région Cantabrique : le Niveau F de la grotte de El Cierro (Ribadesella,Asturies, Espagne)

El Cierro Cave (Ribadesella, Asturias, Spain), located near the mouth of the River Sella, has yielded one of the most important Upper Palaeolithic sequences in northern Spain. To date, three major occupation periods at the cave have been identified and dated. The first was at the beginning of the Holocene (ca. 8500 BP; ca. 9000 cal BP); the second at the end of the Upper Palaeolithic, in the Younger Dryas (YD) or Greenland Stadial 1 (GS1) (ca. 11.200 BP; 12.700 cal BP) and the third during Greenland Stadial 2 (GS2) (ca. 16.300–15.500 BP; ca. 19.200–18.700 cal BP). This paper describes the stratigraphy documented in the excavations performed by F. Jordá Cerdá and A. Gómez-Fuentes between 1977 and 1979 and presents the first radiocarbon determinations for the first two occupation periods, together with the study of the archaeological materials found in Level F. This level, dated to 15.500 BP (ca. 18.700 cal BP) is characterised by specialised red deer hunting and the gathering of marine resources (winkles). Various artefacts made from animal raw materials have been documented; both finished products and items in the process of being manufactured, as well as portable art objects. The lithic assemblage, consisting mainly of local raw materials with a small proportion of allochthonous flint, is characterised by an abundance of small bladelet cores and backed bladelets. These archaeological remains and the radiocarbon date mean Level F can be attributed to the so-called “Cantabrian Lower Magdalenian”. This period has been documented archaeologically and dated to a similar time at other sites in the River Sella valley and in the rest of northern Spain.     

Chronologie du Paléolithique supérieur dans le Nord-Est de la principale île du Japon

Palaeolithic archaeology in Tohoku region has long been discussed on constructing chronology, however it is difficult to build reliable chronological order because of poor stratigraphic excavations. In recent radiocarbon dating has advanced. In this paper I discuss the relation between chronology and radiocarbon dating in Tohoku region. At first, I categorize the Palaeolithic industries and establish the chronology by analyzing tool typology, lithic technology, and stratigraphic data. I correlate it with radiocarbon data from sites in Tohoku region. The result of analysis shows that Upper Palaeolithic industries are divided into 18 categories and 8 periods on chronology. The calibration curve IntCal 13 indicated that oldest Early Upper Palaeolithic site appeared around 37,000 cal BP, and late Upper Palaeolithic started about 27,000 cal BP. The pottery first appeared as far back as around 16,000 cal BP. Now we do not have enough radiocarbon data, so we have to gather and examine more ¹⁴C data.     

Early human occupations at the westernmost tip of Eurasia: The lithic industries from Menez–Dregan I (Plouhinec,Finistère,France)

The stratigraphical complex preserved at the site of Menez–Dregan I (Brittany, France) displays an alternating sequence of 17 occupation levels and of 4 marine deposits, between ca. 450 and 150,000 years (stratigraphical units 9a and 3b). The lithic industry retrieved at the site is extremely abundant, with more than 153,000 artefacts over 3 cm in length, as well as millions of knapping debris, and corresponds to a regional facies of the Acheulean, with heavy-duty tools essentially represented by choppers, as well as a few handaxes and cleavers. This paper presents a first synthesis of the data produced for almost 30 years on the site of Menez–Dregan I. The typological study of the entire lithic collection is now complete and allows us to assess the different human occupations that occurred at this site during the Lower Palaeolithic.     

Études du Paléolithique du Japon à partir des téphras

Many studies and discussions have been made on the problem of when the earliest human beings appeared in Japan. In general, hominid fossils in the latest Pleistocene are not preserved except for coralline limestone sequence in Ryukyu islands, but earlier Paleolithic tools were excavated from volcanic ash soil with a ¹⁴C age of about 30,000–35,000 yr. BP or younger at several archeological sites in almost all Japan. Recent studies, however, show a need for revision and refinement of these ages because calibration techniques have progressed from conventional to calendar ages and high-resolution oxygen isotope chronology has given a global standard sequence. Aïra-Tn tephra (AT), the most important time-marker of the Paleolithic age in Japan, was formerly dated at 21,000–22,000 yr ¹⁴C BP by conventional radiocarbon methods but was dated again at ca. 24,500 yr ¹⁴C BP by accelerated mass spectrometry radiocarbon methods. However, it has been further calibrated to a high-resolution calendar age of 30,000 cal yr. by varve chronology of lake sediments of Suigetsu of central Japan, well matched with combined date between oxygen isotope dates based and calibration from AMS radiocarbon dates. As the earliest Paleolithic tools in south Kanto are found in volcanic ash soil significantly below AT ash and above Sambe-Ikeda ash (SI, ca.46 ka), just above the oxygen isotopic stage 3.3, they are estimated to be dated slightly older than 40 ka. Palaeo-environment at that time is estimated mild to cool climate and relatively low sea level after the oxygen isotope stage 3.3. Sill land bridges between Japan islands and continents have not been formed at major straits. We have not yet obtained useful data for calibration older than ca. 45 ka. Also, correlation of oxygen isotopic fluctuation with the terrestrial sequences is incomplete in Stage 3.     

An example of the consequences of human activities on the evolution of subalpine landscapes

A pollen study at Survilly (2235m asl, 06° 49′ 12″ E, 45° 59′ 24″ N), a small peatbog located on the Anterne mountain (Upper-Arve Valley, French north-western Alps) highlights the local role of human activities in Holocene vegetation dynamics of the currently treeless subalpine belt and the consecutive resumption of erosion. As early as 8890 cal. years BP (± 122), Pinus cembra grew close to the site. Grasslands without shrubs were established at around 4624 ± 86 cal. years BP. Due to human activities, spruces extended little after 3600 cal. BP. The intense grazing that resulted in the current alpine meadows goes back to 1436 cal. years BP (± 81). After 4624 cal. BP three clay layers show that from this period, the erosion became as active as during the first steps of the colonization of the vegetation prior to 10,050 cal. BP. During peat growth only a millimetre of clay at the end of the 9400–9050 cal. BP climatic event was recorded.     

Design,synthesis and biological evaluation of tripeptide boronic acid proteasome inhibitors

A series of tripeptide boronate proteasome inhibitors were designed and synthesized on the basis of our previously built tripeptide aldehyde 3D-QSAR models. All the synthesized compounds were evaluated for their proteasome-inhibitory activities in an isolated 20S rabbit proteasome, and selected compounds were evaluated for their antitumor activities in vitro against four human cancer cell lines. Biological results showed bulky and negative substituents at P² position improved the proteasome-inhibitory potency obviously, which completely conformed to the theoretical models, while those at P³ position thoroughly deviated from the 3D-QSAR model. Most of the screened compounds showed less than 1 nM inhibitory potency and high selectivity against 20S proteasome, of which 7f is the most potent (IC₅₀ = 0.079 nM) and twofold more active than bortezomib (IC₅₀ = 0.161 nM). Cell viability indicated hydrophilic 4-hydroxyphenyl substituent at P² or P³ position was not favorable to the cellular activities. Especially for the two hematologic cancer cell lines, HL-60 and U266, 7f inhibited them at the level of less than 10 nM and was more potent than the control bortezomib. It is being considered a promising new lead to be developed for the treatment of various cancers.     

Les industries lithiques moustériennes de la Baume Moula-Guercy (Soyons,Ardèche). Fouilles 1993–1999

The Moula-Guercy cave is located in southeastern France in the middle part and on the west bank of the Rhone valley, 80 meters above the Pleistocene Rhone River between the Ardeche Mountains and the western part of the Alps. Excavations spanning from 1993–1999 have yielded 2595 lithic artefacts out of which over 92% are coming from the four main layers (lV, VIII, XIV and XV) corresponding to the seasonal hunting site. The stratigraphic sequence is exclusively Middle Paleolithic. Paleontological and geological analysis led to the division of the sequence into 19 layers grouped into three climatic phases corresponding to isotope stages 4 to 6. The layer XV unearthed the remains of 6 cannibalized Neanderthals: children, adolescents, and adults. The study of the lithic assemblages highlights two distinct sets corresponding to layers IV–VIII and XIV–XV. This probably indicates that the same territory was travelled by two human groups with different technical traditions ten thousands years apart in very different climatic and ecological contexts. This study is also questioning whether the discoid debitage (sensu Bordes) should be part of the Levallois philosophy.     

Re-dating the Early Upper Paleolithic Levels of Le Trou Magrite (Pont-à-Lesse,Belgium)

All but one of the published radiocarbon dates from the 1991–1992 excavations of Strata 3 and 2 at le Trou Magrite are considered too recent because the dating was done with then-standard chemical pretreatment protocols. This study re-dates Stratum 2 using the same, then-pioneering, XAD-2 purification method on bone collagen as had been used for the 44,650 cal BP date from Stratum 3. The results are two averaged dates that are in stratigraphic order between themselves and in relation to the Stratum 3 date: 43,400 and 43,500 cal BP, according to the IntCal20 curve. These dates are very similar to recently published dates for the earliest Aurignacian in SW Germany and the latest Neanderthal remains in Belgium and they are associated with artifact assemblages that, without obvious evidence of mixture (other than that which was highly localized), include Upper Paleolithic stone tools and blades/bladelets together with numerous sidescrapers, denticulates and notches which are not exclusively Mousterian artifacts. Nineteenth-century excavations in the cave of le Trou Magrite yielded unambiguously diagnostic Aurignacian artifacts and works of portable art that could conceivably have been from a deposit equivalent in age to these strata on the contiguous terrace. It is clear that the first blade(let)-rich assemblages in the site were created on the cusp of the transition from the Middle-to-Upper Paleolithic transition and replacement of the Neanderthals in NW Europe.     

Oldest art or symbolic expressions in North America? Pleistocene modified bones and a human remain at Sima de las Golondrinas cave,Zacatecas, Mexico

The discovery of Pleistocene human presence at Chiquihuite Cave (state of Zacatecas, Mexico) dating to, or even before, the Last Glacial Maximum (LGM, over 18,000 years ago), prompted the search for another cave site in the same region, where the implications of Chiquihuite could be tested and corroborated in a second context. In January 2020, we started work at Sima de las Golondrinas (“Chasm of Swallows”), a cavern in the Zuloaga mountains. Excavation unit X-20 focused on an older profile left behind by unknown early-20th-century explorers. Previous radiocarbon dating of three charcoal-rich deposits had indicated the stratigraphy contained deposits ranging in age from the Terminal LGM to the Middle Holocene. The short-timed excavation revealed the stratigraphic sequence had been slowly deposited in an aquatic environment, when the cave was partly inundated for thousands of years, until the Holocene. Preliminary palynological studies confirmed the presence of water and nearby lakes, matching the paleoenvironmental reconstructions from Chiquihuite, 100 km away. Excavation X-20 yielded no lithic tools or stone raw materials, but an abundance of zoo-archaeological materials, yet without the presence of traditional megafauna. Some specimens present human modifications in the form of butchery-related cut marks, but also engravings possibly related to early symbolic behaviors. Here, we present a selection of eight bones of elevated archaeological importance. One of them is an ischium bone belonging to a young Homo sp. individual, dating to the Early Holocene. The other seven are modified bones coming from layers dating between the Terminal LGM and Younger Dryas. They belonged to white-tailed deer (Odocoileus virginianus), mountain bighorn sheep (Ovis canadensis), and American pronghorn (Antilocapra americana). The assemblage includes four human-modified animal phalanges, with symbolic expression substrates. Two of them were found in levels older than 16,000 years, and may well represent some of the oldest forms of art in the Americas.     

New palaeoanthropological research in the Plio-Pleistocene Omo Group,Lower Omo Valley,SNNPR (Southern Nations,Nationalities and People Regions), Ethiopia

Through previous works in the early 1930s by C. Arambourg and in the 1960–1970s by the International Omo Research Expedition (IORE) initiated by F. C. Howell, the Omo Group deposits of the Lower Omo Valley provided decisive data on Plio-Pleistocene environmental change and hominid evolution in eastern Africa. Y. Coppens directed the IORE French component with Arambourg, then alone from 1970 to 1976. After 30-year hiatus, the Omo Group Research Expedition reinitiated field work on Shungura Formation deposits aged between 3 Ma and 2 Ma. In 2006 and 2007, renewed methods led to the collection of more than 600 vertebrate specimens with a particularly precise record of contextual data. These specimens include significant hominid remains dated to 2.5 Ma and slightly older. Changes in faunal distributions were also recorded. Additionally, the Shungura Formation archaeological record is reconsidered. These first results are indicative of future advances in the study of biodiversity evolution and its relationship with global and regional environmental changes.     

The major Arabidopsis thaliana apurinic/apyrimidinic endonuclease,ARP is involved in the plant nucleotide incision repair pathway

Apurinic/apyrimidinic (AP) endonucleases are important DNA repair enzymes involved in two overlapping pathways: DNA glycosylase-initiated base excision (BER) and AP endonuclease-initiated nucleotide incision repair (NIR). In the BER pathway, AP endonucleases cleave DNA at AP sites and 3'-blocking moieties generated by DNA glycosylases, whereas in NIR, the same AP endonucleases incise DNA 5' to a wide variety of oxidized bases. The flowering plant Arabidopsis thaliana contains three genes encoding homologues of major human AP endonuclease 1 (APE1): Arp, Ape1L and Ape2. It has been shown that all three proteins contain AP site cleavage and 3'-repair phosphodiesterase activities; however, it was not known whether the plant AP endonucleases contain the NIR activity. Here, we report that ARP proteins from Arabidopsis and common wheat (Triticum aestivum) contain NIR and 3' → 5' exonuclease activities in addition to their AP endonuclease and 3'-repair phosphodiesterase functions. The steady-state kinetic parameters of reactions indicate that Arabidopsis ARP cleaves oligonucleotide duplexes containing α-anomeric 2'-deoxyadenosine (αdA) and 5,6-dihydrouridine (DHU) with efficiencies (k_cat/K_M = 134 and 7.3 μM⁻¹·min⁻¹, respectively) comparable to those of the human counterpart. However, the ARP-catalyzed 3'-repair phosphodiesterase and 3' → 5' exonuclease activities (k_cat/K_M = 314 and 34 μM⁻¹·min⁻¹, respectively) were about 10-fold less efficient as compared to those of APE1. Interestingly, homozygous A. thaliana arp^–/– mutant exhibited high sensitivity to methyl methanesulfonate and tert-butyl hydroperoxide, but not to H₂O₂, suggesting that ARP is a major plant AP endonuclease that removes abasic sites and specific types of oxidative DNA base damage. Taken together, these data establish the presence of the NIR pathway in plants and suggest its possible role in the repair of DNA damage generated by oxidative stress.     

Late Pliocene grassland from Olduvai Gorge,Tanzania

The Olduvai fossil plants documented by us in this paper are the first direct evidence for open grassland in the late Neogene of Africa based on macroplant remains. Silicified remains of herbaceous ground cover are exceptionally well preserved in situ within Late Pliocene sediments below the initial pyroclastic ash surge unit of Tuff IF in the uppermost part of Bed I, Olduvai Gorge, northern Tanzania. Published radiometric and palaeomagnetic dates place this grass layer between 1.839 + 0.005 Ma and 1.785 + 0.01 Ma. Exposed at localities on the south side of the Gorge this herbaceous ground cover grew on a floodplain developed on a dried out lake bed, following pronounced lake retreat of saline–alkaline palaeo-Lake Olduvai during a developing dry climatic phase. Sheathed basal culms, rhizomes and roots are interpreted as those of one or more small mat-forming grasses or less likely, sedges. Small dicotyledonous herbs were probably also present. The proximity of adjacent plants indicates a relatively dense ground cover. Roots extended at least 8 cm below the ground surface. Aerial parts of the plants were absent or were not preserved when the weathered basal culms were covered by a thin layer of brown waxy clay, followed by fallout of pyroclastic ash. Both units were mostly eroded away prior to emplacement of a wet, cool pyroclastic surge which then buried and preserved in situ remnants of the herbaceous ground cover. Preservation of the semi-woody rhizomes implies well-drained soils, otherwise the plant material would have quickly rotted. Collections from discontinuous exposures indicate the grassland covered an area of at least a few hectares. This open grassland would have provided grazing for the Late Pliocene fauna.     

Development and validation of a method for the determination of a therapeutic peptide with affinity for the human B1 receptor in human plasma using HPLC-MS/MS

The peptide described in this report (MW 1180 Da; 10-amino acid synthetic peptide) is a potent and selective antagonist of the human B1 receptor (B1) that has been investigated for the treatment of chronic pain. A method to quantitate this peptide in human plasma has been developed to support human clinical trials designed to evaluate the safety, pharmacokinetics, and efficacy of this compound. Plasma samples (0.2 mL) were extracted using a Waters Oasis MAX (10 mg) 96-well plate and the resulting samples were analyzed using an Applied Biosystems API-5000 HPLC-MS/MS with an electrospray ionization (ESI) source. The method was validated for the determination of the B1 peptide in human plasma over the concentration range of 1–50 ng/mL. Isotopically labeled B1 peptide (¹³C6¹⁵N₂-B1 peptide) was used as an internal standard. Interday precision and accuracy, determined from analysis of quality control (QC) samples, yielded coefficients of variation (CV) of less than 5.3% and accuracy within a 2.4%. Within batch precision and accuracy determinations provided CV values of less than 7.3% and accuracy within a 6.0% bias. Precautions had to be taken to prevent B1 peptide loss to container surfaces and contamination of the HPLC-MS/MS. The validated assay was used in support of human clinical trials.