The World’s Oldest Tsunami Victim at the Gateway to the Pacific—and Beyond

The 1998 Papua New Guinea tsunami was a significant puzzle for scientists who finally cracked the cause, but it also marks the most recent event of many that can be dated back to at least 6,000 years ago where the skull of the oldest tsunami victim in the world was found. Papua New Guinea was also the starting point for the most remarkable navigational feat in the world, with Polynesians moving rapidly east into the Pacific Ocean, their settlement of the region being punctuated by hiatuses caused by catastrophic tsunamis approximately 3,000, 2,000, and 600 years ago. It was on isolated Pacific islands that humans first came into contact with the deadly Pacific Ring of Fire. Settlement abandonment, mass graves, and cultural collapse mark their progress.

EXPLAINING VARIABILITY IN ON-FLOOR ASSEMBLAGES: THE BEHAVIORAL-CONTEXTUAL METHOD

We present a behavioral-contextual method for studying abandonment-related assemblages in order to ascribe them to a settlement abandonment scenario. Our approach examines the vertical and horizontal architectural contexts of assemblages, along with the nature of reconstructible vessels and other artifacts. This method accounts for gradual, rapid, mundane, and ceremonial abandonment scenarios, and for abandonment with anticipated return. Two advantages of this model are its replicability and its proposition of a shared taxonomy leading away from the concept of problematic deposits. The method is contextualized with two distinct case studies from the southern Maya lowlands: the palace of La Corona, Guatemala and an agricultural household group from greater Minanha, Belize. These dissimilar but contemporary (ca. A.D. 900) contexts revealed complex abandonment-related assemblages, including pre-abandonment middens, de facto and secondary material, and on-floor, exposed offerings. Both case studies are argued to reflect gradual, organized abandonment scenarios, although with significant temporal and behavioral distinctions.

Precise timing of abrupt increase in dust activity in the Middle East coincident with 4.2 ka social change

The extent to which climate change causes significant societal disruption remains controversial. An important example is the decline of the Akkadian Empire in northern Mesopotamia ∼4.2 ka, for which the existence of a coincident climate event is still uncertain. Here we present an Iranian stalagmite record spanning 5.2 ka to 3.7 ka, dated with 25 U/Th ages that provide an average age uncertainty of 31 y (1σ). We find two periods of increased Mg/Ca, beginning abruptly at 4.51 and 4.26 ka, and lasting 110 and 290 y, respectively. Each of these periods coincides with slower vertical stalagmite growth and a gradual increase in stable oxygen isotope ratios. The periods of high Mg/Ca are explained by periods of increased dust flux sourced from the Mesopotamia region, and the abrupt onset of this dustiness indicates threshold behavior in response to aridity. This interpretation is consistent with existing marine and terrestrial records from the broad region, which also suggest that the later, longer event beginning at 4.26 ka is of greater regional extent and/or amplitude. The chronological precision and high resolution of our record indicates that there is no significant difference, at decadal level, between the start date of the second, larger dust event and the timing of North Mesopotamia settlement abandonment, and furthermore reveals striking similarity between the total duration of the second dust event and settlement abandonment. The Iranian record demonstrates this region’s threshold behavior in dust production, and its ability to maintain this climate state for multiple centuries naturally.