The history and chronology of siwalik cercopithecids

Cercopithecid monkeys make a comparatively late appearance in the Miocene Siwalik formations of the Indian Subcontinent. The oldest well-dated specimen is a 6.3 MY old colobine, ?Presbytis sivalensis, and it is doubtful that any cercopithecids were present in the Siwalik faunas prior to 7.0 MY, a date that is considerably later than estimates for their appearance elsewhere in Eurasia. Cercopithecines appear later than colobines. Although their temporal ranges are uncertain, cercopithecines evidently were not present before 3.2 MY and possibly not until 2.5 MY. They are represented by three species,?Macaca palaeindica, Procynocephalus subhimalayanus, andTheropithecus delsoni. In the Siwaliks the appearances of colobines and cercopithecines coincide with or follow shortly after major faunal changes that also bring other northern Eurasian and African taxa into the region.     

Historical changes in phosphorus accumulation in a small lake

Isotopes like 210Pb and 137Cs are effectivetools for determining chronology in lake sediments. Once the chronology is established, environmentalchanges in lakes can be investigated, and the causesfor those changes can often be inferred. 210Pband 137Cs profiles were constructed for thesediments of Crystal Lake, Connecticut, USA. Thegeochronology was used to determine the historicalchanges in organic matter and P accumulationin the sediment. Those profiles showed twosignificant periods of sedimentation which correlatewith major precipitation events. DecreasingP accumulation in the sediments of the lakein the last decade was also correlated with increasingeutrophication as documented by increases inepilimnetic P and decreases intransparency.     

When and how did the terrestrial mid-Permian mass extinction occur? Evidence from the tetrapod record of the Karoo Basin,South Africa

A mid-Permian (Guadalupian epoch) extinction event at approximately 260 Ma has been mooted for two decades. This is based primarily on invertebrate biostratigraphy of Guadalupian–Lopingian marine carbonate platforms in southern China, which are temporally constrained by correlation to the associated Emeishan Large Igneous Province (LIP). Despite attempts to identify a similar biodiversity crisis in the terrestrial realm, the low resolution of mid-Permian tetrapod biostratigraphy and a lack of robust geochronological constraints have until now hampered both the correlation and quantification of terrestrial extinctions. Here we present an extensive compilation of tetrapod-stratigraphic data analysed by the constrained optimization (CONOP) algorithm that reveals a significant extinction event among tetrapods within the lower Beaufort Group of the Karoo Basin, South Africa, in the latest Capitanian. Our fossil dataset reveals a 74–80% loss of generic richness between the upper Tapinocephalus Assemblage Zone (AZ) and the mid-Pristerognathus AZ that is temporally constrained by a U–Pb zircon date (CA-TIMS method) of 260.259 ± 0.081 Ma from a tuff near the top of the Tapinocephalus AZ. This strengthens the biochronology of the Permian Beaufort Group and supports the existence of a mid-Permian mass extinction event on land near the end of the Guadalupian. Our results permit a temporal association between the extinction of dinocephalian therapsids and the LIP volcanism at Emeishan, as well as the marine end-Guadalupian extinctions.     

A new,high‐precision CA‐ID‐TIMS date for the ‘Kalkberg’ K‐bentonite (Judds Falls Bentonite)

The numerical calibration of the base of the Devonian is poorly constrained due to several factors. Few precise radioisotopic age determinations are available from the late Silurian and Early Devonian, and the limited published data carry large error bars from older analytical methodologies. Volcanic ashfalls suitable for dating occur in the Lower Devonian of the Appalachian Basin, but have not been precisely correlated into the global chronostratigraphical scheme because of limited bio‐ and lithostratigraphical information. Here, we report a new U‐Pb zircon radioisotopic age determination of 417.61 ± 0.12(0.23)[0.50] Ma and improved chronostratigraphical context, including revised biostratigraphy, for an ash bed in the New Scotland Formation, Helderberg Group, from the Lochkovian Stage that was previously identified as the Kalkberg K‐bentonite. This new information helps to integrate the classic New York Appalachian Basin succession into global Siluro‐Devonian stratigraphy, refine the calibration of the Silurian–Devonian boundary and more precisely estimate the duration of both time periods.     

中国古人类遗址年代学的研究进展与问题

我国丰富的古人类遗存为研究东亚乃至全球古人类起源、迁徙和演化提供了重要的基础材料与数据。对已发表的2000多处旧石器时代古人类遗址年代学数据的整理和统计分析发现,绝大多数遗址目前仍缺少基本的年代学数据,不足20%的遗址开展过测年,仅10%左右具有相对可靠的年代学数据,只有极少数开展了多种测年方法的交叉定年。对于80多处出土古人类化石的遗址,亦过半存在明显的年代学争议。我们对一些古人类遗址中的常见各种复杂的同沉积和沉积后改造现象进行了详细分析,探讨了我国测年平台和测年队伍建设、考古发掘以及年代学采样与测年方法学等方面存在的问题,及其对遗址年代学研究的可能影响。基于此,笔者提出改善我国古人类年代学研究现状的可能措施,希望可以抛砖引玉,引发对该研究领域更多的关注和思考。     

Seasonality of sediment skewness as a geochronological tool for the Humber salt marshes,U.K.

Understanding the patterns of marsh growth hasprimarily been based on modeling. Empiricalverifications of such models are difficult. This isattributed to the inability of available techniques togenerate past annual accretion rates from marshsediment cores and the need for an extremely longobservation period if a set of present day accretionrates is to be collected and used for such a purpose.Hypothetically, the large variation in temperaturebetween summer and winter, occurring on some saltmarshes, affects the viscosity of the tidal watersinundating and consequently the characteristics of thesediments deposited on the marsh surface. Thevariability of characteristics between seasonallydeposited sediment can be used as annual markers toderive annual accretion rates. Sedimentationexperiments at various temperatures and detailedanalyses of core sediments, cut at 1 mm. intervals,from two selected Humber marshes, were conducted totest the hypothesis.The sedimentation experiments showed that sedimentskewness, a sedimentological characteristic used toindicate the symmetry of the sediment distributioncurve about the mean, is most sensitive to variationsin water temperature and can be used as annual markersin marsh sediments. Detailed sedimentological analysesof two Humber marsh cores showed skew variabilityfollows a low magnitude cyclicity throughout bothcores. Using a 3 year time lag period and thenegative skew peaks as annual markers, correlationbetween a set of peak negative skew values, occurringwithin a dated section of the core, and the averagesummer field temperatures was found to bestatistically significant. The period for sediment toaccumulate within the dated section was calculated toequal the period derived from the dateable pollutanthorizons respectively. Additionally, the annualaccretion rates derived using the negative skew peaksas annual markers are comparable to the observedaverage annual accretion rates previously reported.     

Fission-track dating in paleoanthropology

During the last 30 years, fission-track dating has become a versatile geochronological tool.¹ Fission-tracks, discovered in the early 1960s,² were subsequently used to determine the age of minerals and glasses.³ Although low track densities can make fission-track dating tedious and time-consuming, the technique can provide important data for material in time ranges as young as the last few million years. In anthropological studies, fission-track dating is most useful for dating burned artifacts and volcanic ashes intercalated with hominid-bearing layers.     

New age constraints on the Middle Stone Age occupations of Kharga Oasis, Western Desert, Egypt

Spring-deposited carbonate rocks, or tufas, exposed along the flanks of the Libyan Plateau near Kharga Oasis, Western Desert, Egypt, can provide a directly datable stratigraphic context for Middle Stone Age/Middle Paleolithic (MSA/MP) archaeological material, if such material can be found in situ within tufa strata. Two such localities (Mata'na Site G and Bulaq Wadi 3 Locus 1) described by Caton-Thompson were revisited and sampled for uranium-series analysis. At Mata'na Site G (KH/MT-02), Middle Stone Age ("Upper Levalloisian") material is underlain by tufa with a uranium-series age of 127.9+/-1.3 ka, and overlain by tufa with an age of 103+/-14 ka. At Bulaq Wadi 3 Locus 1, a uranium-series age of 114.4+/-4.2 ka on tufa capping a small collection of Middle Stone Age artifacts also provides a minimum age constraint on that material. Tufa underlying an MSA workshop (KH/MD-10) indicates that this assemblage, characterized by use of several Levallois reduction methods, was deposited after approximately 124 ka. Furthermore, uranium-series ages averaging approximately 133 ka on a Wadi Midauwara tufa (WME-10) without associated archaeological material suggest that one period of spring flow in the region began during the Marine Isotope Stage 6/5e transition, prior to the warmest portion of the last interglacial period. The dated archaeological material suggests that the distinction that has been identified between Nubian and non-Nubian complexes in the Nile Valley may hold for the Western Desert, although local complexity has yet to be fully described.     

A chronological framework for a long and persistent archaeological record: Melka Kunture, Ethiopia

New ⁴⁰Ar/³⁹Ar geochronological data for several volcanic ash horizons from Melka Kunture, Ethiopia, allow for significantly more precise age constraints to be placed upon the lithostratigraphy, archaeology and paleontology from this long record. Ashes from the Melka Kunture Formation at Gombore yielded the most reliable age constraints, from 1.393 ± 0.162 Ma² (millions of years ago) near the base of the section to 0.709 ± 0.013 Ma near the top. Dating the Garba section proved more problematic, but the base of the section, which contains numerous Oldowan obsidian artifacts, may be >1.719 ± 0.199 Ma, while the top is securely dated to 0.869 ± 0.020 Ma. The large ignimbrite from the Kella Formation at Kella and Melka Garba is dated to 1.262 ± 0.034 Ma and pre-dates Acheulean artifacts in the area. The Gombore II site, which has yielded two Homo skull fragments, ‘twisted bifaces,’ and a preserved butchery site, is now constrained between 0.875 ± 0.010 Ma and 0.709 ± 0.013 Ma. Additional ashes from these and other sites further constrain the timing of deposition throughout the section.Integration with previously published magnetostratigraphy has allowed for the first time a relatively complete, reliable timeline for the deposition of sediments, environmental changes, archaeology, and paleontology at Melka Kunture.