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ch 3: This chapter puts humans in our evolutionary context, answering such “who questions” as we need to answer before investigating “how questions.” First, it explains where we fit in terms of broader patterns of primate evolution. Next, it shows how human behavior differs from that of other animals. Finally, it considers how we humans differ from one another. The most important differences among humans are cultural differences. Culture has several distinct properties for which we should expect to find evidence in the prehistoric record. Failing to find such evidence can suggest problems in our methods for investigating human evolution and prehistory.
This reaction to the Paul Newson and Ruth Young paper entitled ‘Post-conflict ethics, archaeology and archaeological heritage. A call for discussion’ (Archaeological dialogues, 2022) supports the call for a discussion regarding archaeological ethics in post-conflict zones. Following the agreement on the fuzzy border between the state of ‘conflict’ and ‘post-conflict’, it reflects on the continuity between these two. Furthermore, the reaction adds an additional issue to the discussion, which is the ethical ground of ‘being above the conflict’. Applying a ‘holistic ethic’ approach, it reflects on the ethical assessment of archaeological practices performed by Russian archaeologists in the zones that were damaged during conflict, escalated due to the actions of the Russian government. A series of examples are shown to consider the complexity of ethical judgements in this particular case. Last but not least, the reaction claims that in some cases ethical judgements are possible and effective due to the convergence of numerous factors.
ch 14: This chapter reviews what we think we know about how earlier humans established our global diaspora. This evidence consistently refutes the hypothesis that humans migrated before they had storable and transportable food sources, such as those arising from food production. Pleistocene humans did not migrate, they dispersed. To explain these dispersals, this chapter first compares what we can observe about differences between living humans and other animals with what we think we know about the earliest Homo sapiens populations. Next, it argues that humans relied on a suite of ancestral survival skills to overcome the obstacles they faced while dispersing. Finally, the chapter considers near, longer, and longest-term challenges to our survival and what we must do to overcome them.
ch 13: This chapter considers whether Homo sapiens is as “unstoppable” as the Titanic was “unsinkable.” Reviewing scientifically credible threats to our species’ long-term survival, this chapter shows that some threats looming large in the popular imagination are actually extremely unlikely to cause human extinction. Actual threats to long-term human survival, such as meteor impacts and large-scale volcanism, garner far less attention than they deserve and they share a similar solution.
ch 12: This chapter examines prehistoric migrations to oceanic islands. First, it considers the special difficulties of reaching such islands, and reviews claims about Pleistocene preagricultural movement to oceanic islands. Next, it focuses on the peopling of the Pacific Ocean, the fastest and most geographically extensive human population movement of all time. Though some archaeologists have speculated that these islands were colonized accidentally, the evidence shows that these were purposeful voyages by people who knew exactly where they were going and how to get there. Lowered sea levels during the LGM/MIS 2 shortened distances between some islands and possibly aided humans living in Sunda, Wallacea, and Sahul in settling Near Oceania. Movements into Remote Oceania commenced around 4 Ka, and movements into Polynesia after 1 Ka. Finally, the chapter considers future human migrations on Earth and beyond. The latter, it argues, will not be “just like Star Trek.”
Regional offsets from Northern Hemisphere radiocarbon (14C) calibration curves are widely recognized for monsoon Asia and often hinder accurate 14C dating. In this paper, we explore the possible linkage between summer monsoon intensity and 14C offsets using tree-ring δ18O and 14C data from Thailand. We developed a 297-yr floating tree-ring δ18O chronology comprising seven teak log-coffin samples from the Ban Rai rock shelter site, northwestern Thailand. The outermost ring of our chronology was estimated to date from 358–383 CE, within a 95.4% (2σ) probability range, based on a total of 10 14C measurements that were wiggle-matched against a mixed calibration curve evenly weighted from the IntCal20 and SHCal20 curves. Backward trajectory analysis showed that an intensified (weakened) summer monsoon detected in a modern tree-ring δ18O chronology was most likely to be induced by increased (decreased) air mass transport from the tropical Indian Ocean, which is an area of intense upwelling where the 14C concentration is lower than the atmospheric 14C level. However, partly because of the limited sample size and dating uncertainty, the direct linkage between the tree-ring δ18O series and 14C records obtained from our teak log-coffin samples could not be statistically verified.
In a recent Antiquity article, Darvill (2022) proposed that the mid third-millennium BC Stage 2 sarsen settings of Stonehenge (comprising the Trilithon Horseshoe, Sarsen Circle and the Station Stone Rectangle) were conceived in order to represent a calendar year of 365.25 days—that is, a calendar identical in duration to the Julian calendar. In the present article, the authors argue that this proposal is unsubstantiated, being based as it is on a combination of numerology, astronomical error and unsupported analogy.
ch 10: This chapter examines the peopling of the “New World” (Beringia and the Americas) between 12 and 32 Ka. Like the peopling of Sahul, population movements brought Homo sapiens from Asia to American continents and offshore islands with no prior hominin presence. Historically, archaeologists envisioned these movements as land-based, passing through an “ice-free corridor” between major continental glaciers around 13 Ka, but evidence increasingly shows that humans were already present south of the ice sheets significantly earlier than this corridor existed. Unlike in Sahul, ancestral Native Americans systematically hunted many of the megafauna that became extinct during the Pleistocene-Holocene transition. Extensive alliance networks whose most durable archaeological traces include distinctive stoneworking traditions, such as the Clovis Complex, may have played a role in these mass extinctions.
ch 11: This chapter considers the relationship between food production and migration. Before Holocene times (> 12 Ka) archaeological evidence consistently shows that human population movements were dispersals and not migrations. People moved into new habitats either as individuals or in small groups, reconfiguring their economies and social identities in their destinations. From mid-Holocene times onward (after 4–8 Ka), however, the archaeological record begins to show increasing evidence for migrations. Migrating humans took their food and their culture, their “movable feasts,” with them. This chapter argues that recent human migrations result from food production using domesticated plants and animals. It describes how food production altered some of humanity’s responses to the basic six survival problems in ways that not only encourage migrations but also make them easier for archaeologists to detect, albeit within a limited chronological “window of visibility.” A case study from sub-Saharan Africa shows that archeologists can detect prehistoric migrations, but we have to ask different questions about them than traditional “who questions.”
ch 5: This chapter examines African evidence for human origins, behavior, and population movements between 50 and 600 Ka (thousands of years ago). It compares evidence associated with Homo sapiens and H. heidelbergensis. Homo sapiens and H. heidelbergensis solved survival challenges in broadly similar ways, with humans occasionally devoting more time and energy to technology (“technological intensification”). The African evidence is entirely consistent with dispersal, showing not even a hint of migration. This and other evidence suggest humans replaced earlier H. heidelbergensis not by an abrupt evolutionary event originating in one place and radiating outward but instead by a gradual, continent-wide process whose mode and tempo varied widely.