Pleistocene peopling of the Americas

Our species colonized North and South America last of all the major land masses, thereby ending the spread that began a million years earlier when ancestral members of the genus Homo first ventured out of Africa. But who were the first Americans? When did they arrive? Did they come in one migration or many? How quickly and by what adaptive strategies did they move across the environmentally diverse and trackless New World? How do they relate to contemporary native Americans? We have plenty of answers to these questions. Unfortunately, we can't agree which ones are right. This much is certain: the first Americans were Homo sapiens who came from northeast Asia via the Bering Straits (Fig. 1). They may have walked from Siberia to Alaska across Beringia, the land bridge formed when vast Pleistocene glaciers froze 5% of the world's water,¹ lowering global sea levels and exposing the shallow continental shelf between Asia and America. These hunter-gatherers were present throughout the Americas by 11,500 years ago, in time to witness the climatic and ecological changes, including the extinction of thirty-five genera of megafauna, that signalled the end of the Pleistocene. Beyond those bare facts there is controversy. Here, then, is a brief summary of the state of the argument over the peopling of the Americas.     

Relationship of Old World Pseudoxenodon and New World Dipsadinae, with Comments on Underestimation of Species Diversity of Chinese Pseudoxenodon

Assessment of the relationship between Pseudoxenodon and Dipsadinae has been hampered by lack of adequate samples. In this paper, we conducted phylogenetic analyses using two mitochondrial genes （12S and 16S rRNA） and one nuclear gene （c-mos） from thirteen specimens representing two species of Pseudoxenodon, together with 84 sequences of caenophidians and an outgroup sequence of Boa constrictor. Our study suggests that the Southeast Asian genus, Pseudoxenodon forms a robust genetic subclade within South American xenodontines, indicating that at least one lineage within this genus entered or returned to the Old World （OW） from the New World （NW） across the Beringian Land Bridge during the early Tertiary and the warm mid-Miocene. It also reveals the high intraspecific genomic variation within the populations of Pseudoxenodon macrops, indicating that species diversity of Pseudoxenodon in China is likely underestimated.     

Comparing the Detection of Iron-Based Pottery Pigment on a Carbon-Coated Sherd by SEM-EDS and by Micro-XRF-SEM

The same sherd was analyzed using a scanning electron microscope with energy dispersive spectroscopy (SEM-EDS) and a micro X-ray fluorescence tube attached to a scanning electron microscope (Micro-XRF-SEM) to compare the effectiveness of elemental detection of iron-based pigment. To enhance SEM-EDS mapping, the sherd was carbon coated. The carbon coating was not required to produce Micro-XRF-SEM maps but was applied to maintain an unbiased comparison between the systems. The Micro-XRF-SEM analysis was capable of lower limits of detection than that of the SEM-EDS system, and therefore the Micro-XRF-SEM system could produce elemental maps of elements not easily detected by SEM-EDS mapping systems. Because SEM-EDS and Micro-XRF-SEM have been used for imaging and chemical analysis of biological samples, this comparison of the detection systems should be useful to biologists, especially those involved in bone or tooth (hard tissue) analysis.     

The Good Old Days Were Better: Agrarian Collapse and Tectonics

The theory of plate tectonics contends that the continental plates occupied by humanity are in motion. The hypothesis of agrarian collapse (HAC) holds that gradual, as well as seismic, earth movement can induce ground slope change and modify land-to-sea level relationships, thereby altering the distribution of surface and subsurface runoff, which can lead to abandonment of agricultural land. Mechanical principles underlying ongoing abandonment are detailed for large-scale irrigation systems of the Andean Cordillera Negra. These principles are compatible with a historical scenario integrating urban development at pre-Hispaic Chan Chan, capital of the Chimor polity, with expansion, reform, and collapse of the city's agricultural hinterland. The applicability of the mechanics of agrarian collapse to two other centers of past civilization is briefly considered.     

Biocenoses of Anadyr Estuary (Bering Sea) and conditions of their existence

Some bottom biocenoses in the river mouth area of Anadyr Estuary are studied. Seasonal biocenosis of filamentous algae Acrosiphonia spp. occurs in the intertidal zone, biocenosis of the bivalve Macoma balthica is common at a depth of 4–8 m. Species diversity increases with depth. The distribution of biocenoses and population structure depend on the hydrological regime and substrate type in the surveyed area.     

Lithic microwear analysis in archeology

Stone tools are the most durable and ubiquitous residue of prehistoric hominid activity. For this reason, archeologists attempt to learn as much as possible about hominid behavior from the analysis of lithic artifacts. Lithic microwear analysis reconstructs aspects of stone-tool use from patterned variation in the traces of microscopic wear on those tools. The analysis of lithic microwear traces has increased our understanding of how stone tools were used in contexts ranging from the early Pleistocene to the ethnographic present.