Occurrence of Overall Corded Pottery in the Upper Ottawa Valley, Canada

1963 ◽  
Vol 29 (1) ◽  
pp. 114-115 ◽  
Author(s):  
B. M. Mitchell
Keyword(s):  
New York ◽  
Middle Woodland ◽  
Radiocarbon Dates ◽  
Eastern Ontario ◽  
A Site

AbstractPottery with overall cording as the only form of decoration (both internally and externally) is reported from a site in eastern Ontario. This pottery came from a level overlain by a Middle Woodland component. As overall cording is not a Hopewellian trait, and as Hopewellian is believed to have influenced Woodland, it will be of interest to determine the age of this early level. Radiocarbon dates from this level, when compared with dates from similar culture levels in New York, should throw light on the direction of the spread of corded pottery into the Northeast.

The millennia-long use history of triangular bifaces

2020 ◽  
Vol 41 (4) ◽  
pp. 168-207
Author(s):  
R Michael Stewart
Keyword(s):  
New York ◽  
Future Research ◽  
Middle Woodland ◽  
Late Archaic ◽  
Delaware Valley ◽  
Radiocarbon Dates ◽  
Projectile Points ◽  
Early Woodland ◽  
Middle Archaic ◽  
History Of

Relatively small, triangular bifaces often considered to be projectile points have a demonstrable use history that includes the Middle Archaic, Late Archaic, Early Woodland, late Middle Woodland, Late Woodland, and Contact periods of regional archaeology. Radiocarbon dates and other data are used to document this extensive history using the Upper Delaware Valley of New Jersey, Pennsylvania, and New York as a case study. Observed trends are evaluated in a broader regional context. The degree to which triangles of different ages can be distinguished from one another is addressed and suggestions for future research are made.

Jazz Bubble

2018 ◽  
Author(s):  
Dale Chapman
Keyword(s):  
New York ◽  
Political Economy ◽  
Social Practice ◽  
Global Economy ◽  
First Century ◽  
Music Culture ◽  
Social Trends ◽  
Governmental Organizations ◽  
Early Twenty ◽  
A Site

Hailed by corporate, philanthropic, and governmental organizations as a metaphor for democratic interaction and business dynamics, contemporary jazz culture has a story to tell about the relationship between political economy and social practice in the era of neoliberal capitalism. The Jazz Bubble approaches the emergence of the neoclassical jazz aesthetic since the 1980s as a powerful, if unexpected, point of departure for a wide-ranging investigation of important social trends during this period. The emergence of financialization as a key dimension of the global economy shapes a variety of aspects of contemporary jazz culture, and jazz culture comments upon this dimension in turn. During the stateside return of Dexter Gordon in the mid-1970s, the cultural turmoil of the New York fiscal crisis served as a crucial backdrop to understanding the resonance of Gordon’s appearances in the city. The financial markets directly inform the structural upheaval that major label jazz subsidiaries must navigate in the music industry of the early twenty-first century, and they inform the disruptive impact of urban redevelopment in communities that have relied upon jazz as a site of economic vibrancy. In examining these issues, The Jazz Bubble seeks to intensify conversations surrounding music, culture, and political economy.

Below-the-Watertable Archaeology at Lamoka Lake

1983 ◽  
Vol 4 (2) ◽  
pp. 127-139 ◽  
Author(s):  
Richard Michael Gramly
Keyword(s):  
New York ◽  
New York State ◽  
Middle Woodland ◽  
Late Archaic ◽  
York State ◽  
Animal Bones ◽  
Central New York ◽  
Lake Site

A trench excavated into the waterlogged fringe of the Lamoka Lake site in central New York state yielded cultural stratigraphic zones with abundant artifacts and food remains. A peaty layer resting upon Late Archaic beach or streamside deposits produced late Middle Woodland (Kipp Island phase) ceramics and stone implements. Discoveries of wood, fruit pits, and nuts in the same layer as well as rich congeries of animal bones indicate that the archaeological potential of the Lamoka Lake site is not exhausted.

scholarly journals Balancing Memory and Material at the Lower East Side Tenement Museum

2018 ◽  
Vol 12 (1) ◽  
pp. 14-29
Author(s):  
Gabrielle A. Berlinger
Keyword(s):  
New York ◽  
Material Culture ◽  
Social History ◽  
Ethnographic Study ◽  
Lower East Side ◽  
East Side ◽  
The Public ◽  
Intangible Heritage ◽  
Time Capsule ◽  
A Site

Abstract: Founded in a nationally landmarked apartment building on the ever-gentrifying Lower East Side of Manhattan, New York, the Lower East Side Tenement Museum is an historic site of immigrant social history and material culture. Constructed in 1864 and occupied by over 7,000 immigrants until its closing in 1935, this building has withstood constantly rising visitorship each year since its opening as a museum in 1988. With apartment spaces restored for the public to explore without roped-off restriction, this time capsule of domestic immigrant life requires continual maintenance to preserve its historic physical fabric. Through interviews with the Museum staff and the Preservation Advisory Committee (conservators, architectural historians, curators), as well as documentation of technical processes carried out in the preservation process, this ethnographic study investigates the questions and compromises that arise in the preservation of the tangible and intangible heritage contained within an historic structure in constant use. Which narratives are reconstructed through the Museum’s decisions to restore certain material features of the building while allowing others to decay? What are best practices for interpretation and preservation when a museum’s success results in the gradual destruction of its main artifact (the building) through use? This study explores the intersection of museum mission and practice, heritage construction, and historic preservation at a site both sustained and destroyed by its increasing success.

Geoarchaeology and Bayesian Statistical Modeling of Radiocarbon Dates from 40CH171, a Multicomponent Shell-Bearing Site in Cheatham County, Tennessee

2019 ◽  
pp. 75-90
Author(s):  
D. Shane Miller ◽  
Thaddeus G. Bissett ◽  
Tanya M. Peres ◽  
David G. Anderson ◽  
Stephen B. Carmody ◽  
...  
Keyword(s):  
Site Formation ◽  
State University ◽  
Radiocarbon Dates ◽  
University Of Tennessee ◽  
Middle Tennessee State University ◽  
Blue Creek ◽  
Middle Archaic ◽  
Cumberland River ◽  
A Site ◽  
The University

Using multiple lines of evidence from 40CH171, including opportunistic sampling, geoarchaeology analysis, and Bayesian radiocarbon modeling, this chapter constructs a site formation process narrative based on fieldwork conducted from 2009 to 2010 by the University of Tennessee, Middle Tennessee State University, and the Tennessee Division of Archaeology. This chapter argues that the shell-bearing strata were deposited relatively close to an active channel of the Cumberland River and/or Blue Creek during the Middle Holocene (ca. 7170–6500 cal BP). This was followed by an abrupt shift to sandier sediments, indicating that deposition after the termination of the shell-bearing deposits at the Middle Archaic/Late Archaic boundary took place in the context of decreasing distance from the site to the Cumberland River and Blue Creek.

Mn-Mg disordering in cummingtonite: a high-temperature neutron powder diffraction study

2000 ◽  
Vol 64 (2) ◽  
pp. 255-266 ◽  
Author(s):  
J. J. Reece ◽  
S. A. T. Redfern ◽  
M. D. Welch ◽  
C. M. B. Henderson
Keyword(s):  
Crystal Structure ◽  
Phase Transition ◽  
New York ◽  
High Temperature ◽  
Powder Diffraction ◽  
Elevated Temperatures ◽  
Neutron Powder Diffraction ◽  
Site Preference ◽  
A Site

AbstractThe crystal structure of a manganoan cummingtonite, composition [M4](Na0.13Ca0.41Mg0.46Mn1.00) [M1,2,3](Mg4.87Mn0.13)(Si8O22)(OH)2, (Z = 2), a = 9.5539(2) Å, b = 18.0293(3) Å, c = 5.2999(1) Å, β = 102.614(2)° from Talcville, New York, has been refined at high temperature using in situ neutron powder diffraction. The P21/m to C2/m phase transition, observed as spontaneous strains +ε1 = −ε2, occurs at ˜107°C. Long-range disordering between Mg2+ and Mn2+ on the M(4) and M(2) sites occurs above 550°C. Mn2+ occupies the M(4) and M(2) sites preferring M(4) with a site-preference energy of 24.6±1.5 kJ mol−1. Disordering induces an increase in XMnM2 and decrease in XMnM4 at elevated temperatures. Upon cooling, the ordered states of cation occupancy are ‘frozen in’ and strains in lattice parameters are maintained, suggesting that re-equilibration during cooling has not taken place.

scholarly journals Tree-Ring Records of Near-Younger Dryas Time in Central North America—Preliminary Results from the Lincoln Quarry Site, Central Illinois, Usa

Radiocarbon ◽  
2004 ◽  
Vol 46 (2) ◽  
pp. 933-941 ◽  
Author(s):  
Irina P Panyushkina ◽  
Steven W Leavitt ◽  
Alex Wiedenhoeft ◽  
Sarah Noggle ◽  
Brandon Curry ◽  
...  
Keyword(s):  
North America ◽  
Tree Ring ◽  
Environmental Changes ◽  
Ring Width ◽  
Younger Dryas ◽  
Late Glacial ◽  
Radiocarbon Dates ◽  
Initial Sampling ◽  
Central Illinois ◽  
A Site

The abrupt millennial-scale changes associated with the Younger Dryas (YD) event (“chronozone”) near the dawn of the Holocene are at least hemispheric, if not global, in extent. Evidence for the YD cold excursion is abundant in Europe but fairly meager in central North America. We are engaged in an investigation of high-resolution environmental changes in mid-North America over several millennia (about 10,000 to 14,000 BP) during the Late Glacial–Early Holocene transition, including the YD interval. Several sites containing logs or stumps have been identified and we are in the process of initial sampling or re-sampling them for this project. Here, we report on a site in central Illinois containing a deposit of logs initially thought to be of YD age preserved in alluvial sands. The assemblage of wood represents hardwood (angiosperm) trees, and the ring-width characteristics are favorable to developing formal tree-ring chronologies. However, 4 new radiocarbon dates indicate deposition of wood may have taken place over at least 8000 14C yr (6000–14,000 BP). This complicates the effort to develop a single floating chronology of several hundred years at this site, but it may provide wood from a restricted region over a long period of time from which to develop a sequence of floating chronologies, the timing of deposition and preservation of which could be related to paleoclimatic events and conditions.

Manganese as a site factor for epiphytic lichens

2005 ◽  
Vol 37 (5) ◽  
pp. 409-423 ◽  
Author(s):  
Markus HAUCK ◽  
Alexander PAUL
Keyword(s):  
New York ◽  
New York State ◽  
Membrane Damage ◽  
Coniferous Forests ◽  
Epiphytic Lichens ◽  
Mn Toxicity ◽  
Site Factor ◽  
Manganese Uptake ◽  
A Site ◽  
Mn Concentrations

Decreasing abundance of epiphytic lichens with increasing Mn supply from the substratum or from stemflow was found in several coniferous forests of Europe (Germany) as well as western (Montana, British Columbia) and eastern North America (New York State). Experiments carried out with Hypogymnia physodes and other species of chloro- and cyano-lichens suggest that these correlations are causal. High Mn concentrations e.g. reduce chlorophyll concentrations, chlorophyll fluorescence and degrade the chloroplast in lichen photobionts. Excess Mn inhibits the growth of soredia of H. physodes and causes damage in the fine- and ultra-structure of the soredia. Adult lichen thalli remain structurally unaffected by Mn. Manganese uptake does not result in membrane damage. Calcium, Mg, Fe and perhaps also Si alleviate Mn toxicity symptoms in H. physodes. Lecanora conizaeoides is not sensitive to Mn in laboratory experiments or in the field. The data suggest that high Mn concentrations are an important site factor for epiphytic lichens in coniferous forests that until recently has been overlooked. Manganese reaching the microhabitat of epiphytic lichens is primarily soil-borne and is usually not derived from pollution.

Radiocarbon Dating the Iroquoian Occupation of Northern New York

2019 ◽  
Vol 84 (4) ◽  
pp. 748-761 ◽  
Author(s):  
Timothy J. Abel ◽  
Jessica L. Vavrasek ◽  
John P. Hart
Keyword(s):  
New York ◽  
Population Growth ◽  
Bayesian Analysis ◽  
High Precision ◽  
Radiocarbon Dating ◽  
Faunal Remains ◽  
Radiocarbon Dates

The results of Bayesian analysis using 43 new high-precision AMS radiocarbon dates on maize, faunal remains, and ceramic residues from 18 precontact Iroquoian village sites in Northern New York are presented. Once thought to span AD 1350–1500, the period of occupation suggested by the modeling is approximately AD 1450–1510. This late placement now makes clear that Iroquoians arrived in the region approximately 100 years later than previously thought. This result halves the time in which population growth and significant changes in settlement occurred. The new chronology allows us to better match these events within a broader Northeast temporal framework.

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