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1. Moss kill dates and modeled summer temperature track episodic snowline lowering and ice cap expansion in Arctic Canada through the Common Era

   https://doi.org/10.5194/cp-19-2341-2023  

   Miller, Gifford H; Pendleton, Simon L; Jahn, Alexandra; Zhong, Yafang; Andrews, John T; Lehman, Scott J; Briner, Jason P; Raberg, Jonathan H; Bueltmann, Helga; Raynolds, Martha; et al (January 2023, Climate of the Past)

   Abstract. Most extant ice caps mantling low-relief Arctic Canada landscapes remained cold based throughout the late Holocene, preserving in situ bryophytes killed as ice expanded across vegetated landscapes. After reaching peak late Holocene dimensions ∼1900 CE, ice caps receded as Arctic summers warmed, exposing entombed vegetation. The calibrated radiocarbon ages of entombed moss collected near ice cap margins (kill dates) define when ice advanced across the site, killing the moss, and remained over the site until the year of their collection. In an earlier study, we reported 94 last millennium radiocarbon dates on in situ dead moss collected at ice cap margins across Baffin Island, Arctic Canada. Tight clustering of those ages indicated an abrupt onset of the Little Ice Age at ∼1240 CE and further expansion at ∼1480 CE coincident with episodes of major explosive volcanism. Here we test the confidence in kill dates as reliable predictors of expanding ice caps by resampling two previously densely sampled ice complexes ∼15 years later after ∼250 m of ice recession. The probability density functions (PDFs) of the more recent series of ages match PDFs of the earlier series but with a larger fraction of early Common Era ages. Post 2005 CE ice recession has exposed relict ice caps that grew during earlier Common Era advances and were preserved beneath later ice cap growth. We compare the 106 kill dates from the two ice complexes with 80 kill dates from 62 other ice caps within 250 km of the two densely sampled ice complexes. The PDFs of kill dates from the 62 other ice caps cluster in the same time windows as those from the two ice complexes alone, with the PDF of all 186 kill dates documenting episodes of widespread ice expansion restricted almost exclusively to 250–450 CE, 850–1000 CE, and a dense early Little Ice Age cluster with peaks at ∼1240 and ∼1480 CE. Ice continued to expand after 1480 CE, reaching maximum dimensions at ∼1880 CE that are still visible as zones of sparse vegetation cover in remotely sensed imagery. Intervals of widespread ice cap expansion coincide with persistent decreases in mean summer surface air temperature for the region in a Community Earth System Model (CESM) fully coupled Common Era simulation, suggesting the primary forcings of the observed snowline lowering were both modest declines in summer insolation and cooling resulting from explosive volcanism, most likely intensified by positive feedbacks from increased snow cover and sea ice and reduced northward heat transport by the oceans. The clusters of ice cap expansion defined by moss kill dates are mirrored in an annually resolved Common Era record of ice cap dimensions in Iceland, suggesting this is a circum-North-Atlantic–Arctic climate signal for the Common Era. During the coldest century of the Common Era, 1780–1880 CE, ice caps mantled >11 000 km2 of north-central Baffin Island, whereas <100 km2 is glaciated at present. The peak Little Ice Age state approached conditions expected during the inception phase of an ice age and was only reversed after 1880 CE by anthropogenic alterations of the planetary energy balance. 

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2. Refined Radiocarbon Chronologies for Northern Iroquoian Site Sequences: Implications for coalescence, conflict, and the reception of European goods.

   https://doi.org/doi:10.1017/aaq.2020.73  

   Birch, Jennifer (January 2021, American antiquity)

   null (Ed.)

   This article presents results to date of the Dating Iroquoia project. Our objective is to develop high-precision radiocarbon chronologies for northeastern North American archaeology. Here, we employ Bayesian chronological modeling of 184 AMS radiocarbon dates derived from 42 Northern Iroquoian village sites in five regional sequences in order to construct new date estimates. The resulting revised chronology demands a rethinking of key assumptions about cultural process in the region regarding the directionality and timing of processes of coalescence and conflict and the introduction of European trade goods. The results suggest that internal conflict may have preceded confederacy formation among the Haudenosaunee but not the Wendat, as has been previously assumed. External conflict, previously thought to have begun in the early seventeenth century, began more than a century earlier. New data also indicate that the timing and distribution of European materials were more variable between communities than acknowledged by the logic underlying traditional trade-good chronologies. This enhanced chronological resolution permits the development and application of archaeological theories that center the lived experiences and relational histories of Iroquoian communities, as opposed to the generalized thinking that has dominated past explanatory frameworks 

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3. Zooarchaeological assemblages contextualize the historical ecology and harvest of fur-bearing mammals in Vermont

   https://doi.org/10.3389/fevo.2023.1065567  

   Mychajliw, Alexis M.; Hsi, Audrey Y.; An-Pham, Drew; Olson, Olivia L.; Carder, Nanny; Crock, John G.; Robinson, Francis “Jess” (April 2023, Frontiers in Ecology and Evolution)

   Shifting baselines can skew species harvest guidelines and lead to potentially inaccurate assessments of population status and range. The North American Fur Trade (~1600–1900 CE) profoundly impacted the continent’s socio-ecological systems, but its legacies are often not incorporated in management discussions. We apply a conservation paleobiology lens to address shifting baselines of nine species of fur-bearing mammals in Vermont, including seven mesocarnivores and two semi-aquatic rodents. Using a database maintained by the Vermont Division for Historic Preservation, we identified 25 existing radiocarbon dates of fur-bearer associated features from 16 archaeological localities spanning the Early-Late Holocene. We also generated 7 new radiocarbon dates on beaver and muskrat bones from the Ewing (VT-CH-005), Bohannon (VT-GI-026), and Chimney Point (VT-AD-329) localities. Our new radiocarbon dates cluster within the Late Holocene, immediately prior to and throughout the European contact period, and overlap with The Beaver Wars. We recover a ~8,000 year record of beaver harvest, affirming the millennial scale importance of beavers, a species that is often the focus of human-wildlife conflict research. Comparison of zooarchaeological occurrences with digitized natural history specimens and community science observations reveals geographic range continuity for most species except for the American marten, which was historically extirpated, and confirms the native status of the red fox. While taphonomic constraints make our dataset a conservative assessment, our case studies demonstrate how wildlife managers can employ zooarchaeological data to better understand long-term properties of coupled socio-ecological systems and highlight the cultural importance of these species to Indigenous trade networks prior to the Fur Trade in Vermont. 

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4. Analysis of the earliest complete mtDNA genome of a Caribbean colonial horse (Equus caballus) from 16th-century Haiti

   https://doi.org/10.1371/journal.pone.0270600  

   Delsol, Nicolas; Stucky, Brian J.; Oswald, Jessica A.; Reitz, Elizabeth J.; Emery, Kitty F.; Guralnick, Robert (July 2022, PLOS ONE)

   Chiang, Tzen-Yuh (Ed.)

   Unlike other European domesticates introduced in the Americas after the European invasion, equids (Equidae) were previously in the Western Hemisphere but were extinct by the late Holocene era. The return of equids to the Americas through the introduction of the domestic horse ( Equus caballus ) is documented in the historical literature but is not explored fully either archaeologically or genetically. Historical documents suggest that the first domestic horses were brought from the Iberian Peninsula to the Caribbean in the late 15 th century CE, but archaeological remains of these early introductions are rare. This paper presents the mitochondrial genome of a late 16 th century horse from the Spanish colonial site of Puerto Real (northern Haiti). It represents the earliest complete mitogenome of a post-Columbian domestic horse in the Western Hemisphere offering a unique opportunity to clarify the phylogeographic history of this species in the Americas. Our data supports the hypothesis of an Iberian origin for this early translocated individual and clarifies its phylogenetic relationship with modern breeds in the Americas. 

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5. Resolving Indigenous village occupations and social history across the long century of European permanent settlement in Northeastern North America: The Mohawk River Valley ~1450-1635 CE

   https://doi.org/10.1371/journal.pone.0258555  

   Manning, Sturt W.; Lorentzen, Brita; Hart, John P. (October 2021, PLOS ONE)

   Biehl, Peter F. (Ed.)

   The timeframe of Indigenous settlements in Northeast North America in the 15 th -17 th centuries CE has until very recently been largely described in terms of European material culture and history. An independent chronology was usually absent. Radiocarbon dating has recently begun to change this conventional model radically. The challenge, if an alternative, independent timeframe and history is to be created, is to articulate a high-resolution chronology appropriate and comparable with the lived histories of the Indigenous village settlements of the period. Improving substantially on previous initial work, we report here high-resolution defined chronologies for the three most extensively excavated and iconic ancestral Kanienʼkehá꞉ka (Mohawk) village sites in New York (Smith-Pagerie, Klock and Garoga), and a fourth early historic Indigenous site, Brigg’s Run, and re-assess the wider chronology of the Mohawk River Valley in the mid-15 th to earlier 17 th centuries. This new chronology confirms initial suggestions from radiocarbon that a wholesale reappraisal of past assumptions is necessary, since our dates conflict completely with past dates and the previously presumed temporal order of these three iconic sites. In turn, a wider reassessment of northeastern North American early history and re-interpretation of Atlantic connectivities in the later 15 th through early 17 th centuries is required. Our new closely defined date ranges are achieved employing detailed archival analysis of excavation records to establish the contextual history for radiocarbon-dated samples from each site, tree-ring defined short time series from wood charcoal samples fitted against the radiocarbon calibration curve (‘wiggle-matching’), and Bayesian chronological modelling for each of the individual sites integrating all available prior knowledge and radiocarbon dating probabilities. We define (our preferred model) most likely (68.3% highest posterior density) village occupation ranges for Smith-Pagerie of ~1478–1498, Klock of ~1499–1521, Garoga of ~1550–1582, and Brigg’s Run of ~1619–1632. 

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