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  <dc:title xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Quartz Lake, Alaska 11,200 Year Chironomid and Stable Isotope Data</dc:title>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Wooller, M.J.; Kurek, J.; Gaglioti, B.V.; Cwynar, L.C.; Bigelow, N.H.; Reuther, J.D.; Gelvin-Reymiller, C.; Smol, J.P.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Wooller, M.J.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Kurek, J.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Gaglioti, B.V.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Cwynar, L.C.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Bigelow, N.H.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Reuther, J.D.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Gelvin-Reymiller, C.</dc:creator>
  <dc:creator xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Smol, J.P.</dc:creator>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Arctic</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">PAGES Arctic 2k</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/paleolimnology (carbon/nitrogen,sediment,null,dimensionless,null,paleolimnology,null,null,N,null)</dc:subject>
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  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/paleolimnology</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/paleolimnology</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/paleolimnology</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/paleolimnology</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">earth science/paleoclimate/paleolimnology</dc:subject>
  <dc:subject xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows"> (Quartz Lake&gt;LATITUDE 64.2133&gt;LONGITUDE -145.8211)</dc:subject>
  <dc:description xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Wetlands and lakes in the Tanana Valley, Alaska, have provided 
important resources for prehistoric humans who inhabited this 
region. We examine an ~11,200 cal yr BP record of environmental 
and paleolimnological changes from Quartz Lake in the middle 
Tanana Valley. Our data are also presented in the context of 
recent archaeological findings in the lake&apos;s general vicinity 
that have 18 associated AMS 14C dates. We analyzed the stable-
carbon and nitrogen isotope composition of total organic matter 
from the core, coupled with oxygen and carbon isotope analyses 
of Pisidiidae shells (fingernail clams), in addition to chironomid 
assemblage changes. Lacustrine sediments began to accumulate at 
~11,200 cal yr BP. Initially, autochthonous production was low 
and allochthonous organic input was negligible between 11,000 
and 10,500 cal yr BP, and were associated with relatively cool 
conditions at Quartz Lake at ~10,700 cal yr BP. After 10,500 
cal yr BP, autochthonous production was higher coincident with 
a shift to chironomid assemblages dominated by taxa associated 
with warmer summer climates. A decrease in d13C values of total 
organic carbon (TOC) and organic content of the sediment between 
9,000 and 4,000 cal yr BP may indicate declining autochthonous 
primary production. This period ended with an abrupt (~7 ‰) 
decrease in the d18O values from Pisidiidae shells at ~3,000 
cal yr BP, which we hypothesize represented an episodic 
connection (flood) of the lake with flow from the nearby 
(~6 km) Tanana River. Our findings coincide with evidence for 
major flooding at other locations connected to the Tanana River 
and further afield in Alaska. From ~3,000 cal yr BP Quartz Lake 
subsequently appeared to become a relatively closed system, 
as indicated by the d18OPisidiidae and d13CPisidiidae data 
that are positively correlated and generally higher, 
which also correlates with a shift to moderately higher 
abundances of littoral chironomids. The cause of the transition 
to closed-basin conditions may have been geomorphic rather than 
climatic. This evidence of a progressively stronger evaporative 
influence on the lake&apos;s closed hydrology after ~3,000 cal yr BP 
is consistent with our modern d18O and dD water data from Quartz 
Lake that plot along a regional evaporative line we base on 
isotopic measurements from other local lakes and rivers.  
          STUDY NOTES: Chironomid and stable isotope data from sediments recovered from 
Quartz Lake, Alaska for the past 11,200 years.  

Quartz Lake: 64°12&apos;48&quot;N, 145°49&apos;16&quot;W, 293m elevation </dc:description>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">NCDC-Paleoclimatology</dc:publisher>
  <dc:publisher xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce</dc:publisher>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Wooller, M.J.</dc:contributor>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Kurek, J.</dc:contributor>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Gaglioti, B.V.</dc:contributor>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Cwynar, L.C.</dc:contributor>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Bigelow, N.H.</dc:contributor>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Reuther, J.D.</dc:contributor>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Gelvin-Reymiller, C.</dc:contributor>
  <dc:contributor xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Investigator : Smol, J.P.</dc:contributor>
  <dc:date xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">2012-06-30</dc:date>
  <dc:type xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">ONLINE Files</dc:type>
  <dc:format xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">online, ASCII</dc:format>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/13079</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/alaska/quartz2012.txt</dc:identifier>
  <dc:identifier xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/alaska/quartz2012.xls</dc:identifier>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/alaska/quartz2012.txt</dc:source>
  <dc:source xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/alaska/quartz2012.xls</dc:source>
  <dc:language xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">English</dc:language>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www.ncdc.noaa.gov/paleo/study/13079</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/alaska/quartz2012.txt</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">https://www1.ncdc.noaa.gov/pub/data/paleo/paleolimnology/northamerica/usa/alaska/quartz2012.xls</dc:relation>
  <dc:relation xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">Wooller, M.J., J. Kurek, B.V. Gaglioti, L.C. Cwynar, N. Bigelow, 
J.D. Reuther, C. Gelvin-Reymiller, and J.P. Smol. 2012. 
An ~11,200 year paleolimnological perspective for emerging 
archaeological findings at Quartz Lake, Alaska. 
Journal of Paleolimnology, Vol. 48, No. 1, June 2012, pp. 83-99. 
DOI: 10.1007/s10933-012-9610-9 </dc:relation>
  <dc:coverage xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">START YEAR: 12294 cal yr BP  * END YEAR: 777 cal yr BP</dc:coverage>
  <ows:WGS84BoundingBox xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ows="http://www.opengis.net/ows">
   <ows:LowerCorner>-145.8211  64.2133</ows:LowerCorner>
   <ows:UpperCorner>-145.8211  64.2133</ows:UpperCorner>
  </ows:WGS84BoundingBox>
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