The Carbon-14 Database for Newfoundland and Labrador provides radiocarbon age dates
for over 1400 samples. Data include analytical results from samples collected by the
GSNL, as well as ages from published literature. Radiocarbon ages were obtained
from materials including shells, peat, wood, mud, calcite, charcoal, bone,
gyttja, and faunal remains. Some of the organic and shell samples were collected offshore.
Sample ages are reported as radiocarbon years before present (BP).
It should be assumed that reported ages in this database have not been calibrated to
calendar years before present (with “present” = 1950).
The dates range from modern to older than 40,000 BP, with most occurring between 1,000–14,500 BP.
The limit of carbon-14 dating is currently about 60,000 years; the use of linear accelerators may extend
this limit back to about 100,000 BP.
Users are cautioned that the GSNL radiocarbon database ages have not been assigned confidence or
adjusted based on the sample material type, condition, setting, laboratory pretreatments, contamination
potential, analytical precision at date of publication, field sampling methods, or taphonomic processes.
Ages are reported “as is” from their original publication. We recommend referring to the source publications
to evaluate the appropriateness of individual ages for the user’s specific purpose.
This compilation can be used by geoscientists for a variety of geological purposes,
including studies in relative sea level fluctuations, reconstruction of ice margins, understanding
landscape stability and change, and as a guide for future age-dating work.
Please refer to the Canadian Archaeological Radiocarbon Database (CARD)
overview of "Radiocarbon Dating Principles"
for more detail on radiocarbon dating methodology and limitations.
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Description of Database Attributes and Values (organized alphabetically)
(from Taylor and Batterson, 2001 and Batterson, pers. comm)
14C Date and Associated Error (C14_Date, Pos, Neg):
This column reports radiocarbon age BP, corrected for isotopic fractionation with respect to the D13Cpermil (see below).
The sample date is reported as radiocarbon years before present (BP). This is not equivalent to a calibrated calendar age.
The radiocarbon ages in the database range from modern to greater than 40,000 BP, with most occurring between 1,000–14,000 BP.
The upper limit of radiocarbon dating is typically about 60,000 BP.
All dates have an associated error factor which results from uncertainty related to variability in the production
of radioactive isotopes over time. The date is therefore given as a time interval. Database fields Pos and Neg report
the “plus” and “minus” error bars for the radiocarbon age, respectively, and are also reported in radiocarbon years.
The “true age” will lie within the upper and lower error ranges, with a certain probability. By general convention,
the error range reports one standard deviation (i.e., there is a 68% probability that the true age lies within the
time interval given). However, finite radiocarbon dates from the GSC were reported to within 2 standard deviations
and may be rounded to between 1 and 3 significant figures (see e.g., McNeeley, 2006). Infinite ages (those with no upper limit,
e.g., greater than 34,000 yr BP) from the GSC were reported within 4 standard deviations.
δ13C (D13Cpermil):
This is the isotopic composition of the sample being measured. It represents the parts per thousand difference
(‰) between the sample 13C content and the 13C content of the carbonate in the international
Vienna Pee Dee Belemnite (VPDB) .
VPDB refers to the Cretaceous belemnite formation at Pee Dee in South Carolina, USA. Most 14C samples show
δ13C values about
-25 ‰, and by convention this is the value to which the measured isotopic rations are normalized. Historically, the GSC
took a somewhat different approach: for marine shells, GSC samples were corrected to δ13C = 0 ‰ PDB and then normalized to
δ13C = -25 ‰. This means that GSC dates are about 410 years younger than would be reported from the same sample by another
laboratory. For comparative purposes it is recommended that 410 years be added to GSC ages and the error converted to 1 standard
deviation (Miller et al., 1988).
e = estimated
m = measured
Collector:
This is the name of the sample collector.
Elevation:
Elevation of the sample collection, generally either metres above or below sea level (negative sign).
For lake sediment samples (e.g., gyttja) lake surface elevation is given.
Laboratory Number (LabNum):
This is a unique ID assigned to each database sample that comprises an analytical laboratory identifier,
followed by the sample number (e.g., GSC-4211). The following is a list of laboratory codes:
AA Arizona Accelerator Facility
Beta Beta Analytical, Florida
B Bern, Switzerland
BGS Brock University, Geological Sciences
CAMS Center for Accelerator Mass Spectrometry, USA
DAL Dalhousie University, Halifax
DIC Dicarb Radioisotope Company, Florida
GAK Gakushuin University, Japan
GSC Geological Survey of Canada, Ottawa
GX Geochron Laboratories, Massachusetts
I Teledyne Isotopes, New Jersey
L Lamont, New York
N Nishina Memorial, Japan
P Pennsylvania
Q Godwin Laboratories, Cambridge
S Saskatchewan Research Council
SI Smithsonian Institution, Washington
SM Mobil Oil Corporation, Dallas, USA
St Stockholm, Sweden
T Trondheim, Norway
TO Isotrace Laboratory, University of Toronto
UGa University of Georgia, USA
UQ Universite de Quebec à Montreal
WAT University of Waterloo
Y Yale University
Location:
Sample collection locations are provided as both latitude/longitude and UTM (easting, northing, zone) coordinates.
All coordinates are based on the 1927 North American Datum (NAD27).
Locality:
Locality refers to the named community, lake or pond closest to where the sample was taken.
Material:
The database includes reported ages for a wide range of materials, including: terrestrial and marine shells
and foraminifera; terrestrial and marine macrofauna remains (e.g., bone, charred fat); terrestrial vegetation and
charcoal; peat, detritus, and turf; and sediments including gyttja (total organics), clay, and muds.
The reliability of ages varies with type of sample material, biological or other isotopic fractionation in the environment,
reservoir effects, post-depositional processes, and contamination (often by groundwater). Improvements in the techniques and
calibration curves may also influence age reliability. Reported ages should be evaluated by the user for appropriateness to
address the question at hand.
Reference:
This column reports the source from which the sample age was obtained. Most dates are from the Geological Survey of Canada
(GSC) laboratory, and are listed in the radiocarbon date list published yearly by the GSC. However, if the dates are used in an
alternate publication, that publication is listed in the reference column. Refer to the References/Sources
list below for complete citations.
Uncorrected Age
(Uncor_age):
This is the calculated age of the sample before it was normalized to the VPDB standard ("Vienna Pee Dee Belemnite").
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DISCLAIMER
Open File reports, maps and digital
data issued by the Geological Survey Division of the Mining and Mineral
Development Branch,
Government of Newfoundland and Labrador, are made available for public use. They have not
been formally edited or peer reviewed, and are based
upon preliminary data and evaluation. The user agrees not to provide a
digital reproduction or copy of this product to a third party. Derivative
products should acknowledge the source of the data.
The Geological
Survey, a division of the Mining and Mineral Development Branch, Government of Newfoundland and Labrador
(the "authors and publishers"), retains the sole right to the
original data and information found in any product produced. The authors and
publishers assume no legal liability or responsibility for any alterations,
changes or misrepresentations made by third parties with respect to these
products or the original data. Furthermore, the Geological Survey assumes no
liability with respect to digital reproductions or copies of original products
or for derivative products made by third parties. Please consult with the
Geological Survey in order to ensure originality and correctness of data and/or
products.
RECOMMENDED CITATION
(for downloaded database)
Newfoundland and Labrador Geological Survey. "Radiocarbon Dates."
Newfoundland and Labrador GeoScience Atlas OnLine.
Last update: [check the What's New file].
https://geoatlas.gov.nl.ca [fill in date downloaded].
The original source should be referenced wherever possible. Please refer to the Source citations below or the
Geofiles, to search for the pertinent
reports and maps. The 'Last Update' refers to the last time the
database information was updated and does not refer to cosmetic changes to
the database.
REFERENCES/SOURCES
Compilation:
Taylor, D.M., and Batterson, M.J.
2001: Carbon-14 date list
for Newfoundland and Labrador. Newfoundland Department of Mines and
Energy, Geological Survey, Open File NFLD/2190, version 2. (pdf -
200kb)
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Anderson, T.W.
1983: Preliminary evidence for Late Wisconsinan climatic fluctuations from pollen stratigraphy in Burin Peninsula,
Newfoundland. In Current Research, Part B, Geological Survey of Canada, Paper 83-1B, pages 185-188.
Andrews, J.T., Laymon, C.A. and Briggs, W.M.
1989: Radiocarbon date list III: Labrador and northern Quebec, Canada and Radiocarbon date list VI:
Baffin Island, North West Territories, Canada. Institute of Arctic and Alpine Research, Boulder, Colorado, Occasional paper 46.
Anton, E.P.
2004: St. John's Harbour 5 (HeCi-30) and an Examination of Groswater and Early Dorset Relationships in Labrador.
M.A. thesis, St. John's, Memorial University of Newfoundland, Department of Anthropology.
Auger, R. and Stopp, M.
1989: 1986 archaeological survey of southern Labrador: Quebec/Labrador border to Cape Charles.
Archaeology in Newfoundland and Labrador 1986, Annual Report 7, pages 198-212.
Awadallah S.A. and Batterson M.J.
1990: Comment on "Late deglaciation of the Central Labrador coast and its implications for the age of
glacial lakes Naskaupi and McLean and for pre-history" by P.U. Clark and W.W. Fitzhugh.
Quaternary Research, Volume 34, pages 372-373.
Barrie, C.Q. and Piper, D.J.W.
1982: Late Quaternary marine geology of Makkovik Bay, Labrador. Geological Survey of Canada, Paper 81-17, 37 pages.
Batterson, M.J.
2003: Quaternary geography and sedimentology of the Humber River basin and adjacent areas,
Government of Newfoundland and Labrador, Department of Mines and Energy, Geological Survey,
Report 03-02, 2003, 211 pages.
(pdf - 15 mb)
Batterson, M, and Sheppard, K.
2000: Deglacial history of northern St. Georges Bay, western Newfoundland. in Current Research,
Newfoundland Department of Mines and Energy Geological Survey, Report 2000-1, pages 33-47.
(pdf - 567kb)
Bell, T.
1987: Quaternary geomorphology, glacial history and relative sea level change in outer Nachvak Fiord,
northern Labrador. Unpublished M.Sc. thesis, Memorial University of Newfoundland, St. John's, Nfld.
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2003: A new late‐glacial sea‐level record for St. George's Bay, Newfoundland.
Can. J. Earth Sci., 40(8), 1053– 1070, https://doi.org/10.1139/e03-024
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Geographie physique et Quaternaire, 2005. Vol. 59. n 2-3, p. 129-140. 5 fig., 1 table.
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Berry, J.C. and Drimmie, R.J.
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Blake, W.JR.
1982: Geological Survey of Canada Radiocarbon Dates XXII. Geological Survey of Canada, paper 82-7.
1983: Geological Survey of Canada Radiocarbon Dates XXIII. Geological Survey of Canada, paper 83-7.
1986: Geological Survey of Canada Radiocarbon Dates XXV. Geological Survey of Canada, paper 85-7.
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A thesis submitted to the School of Graduate Studies in partial fulfillment of the requirements for the
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1973: Late Wisconsinan glaciation of southwestern Newfoundland (with special reference to the Stephenville map-area).
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Canadian Journal of Earth Sciences, Volume 14, pages 2101-2120.
1977b: Radiocarbon age of Robinsons Head Moraine, west Newfoundland, and its significance for postglacial sea level changes.
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1972: Isotopes' radiocarbon measurements IX. Radiocarbon 14(1), pages 114-139.
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2000: Late Holocene sea-level changes, eastern Newfoundland. in Current Research (2000)
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Clark, P.U.
1984: Glacial geology of the Kangalaksiorvik-Abloviak region, northern Labrador, Canada.
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Clark, P.U. and Fitzhugh, W.W.
1990: Late deglaciation of the central Labrador coast and its implications for the age of glacial lakes
Naskaupi and McLean and for pre-history. Quaternary Research, Volume 34, pages 296-305.
Clark, P.U. and Josenhans, H.W.
1986: Late Quaternary land-sea correlations, northern Labrador and Labrador Shelf.
Geological Survey of Canada, Paper 86-1B, pages 171-178.
Cox, S.L.
1977: Prehistoric settlement and culture change at Okak, Labrador. Cambridge: Harvard University,
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1980: Dorset settlement and subsistence in northern Labrador. Arctic, volume 33(3): pages 659-669.
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1984: Diverse furres and deeres flesh' - animal use by a 17th century Beothuk population at Boyd's Cove,
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unpublished manuscript.
Cumming, E.H., Aksu, A.E. and Mundie, P.J.
1992: Late Quaternary glacial and sedimentary history of Bonivista Bay, northeast Newfoundland.
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1987: The microstratigraphy of two peat sequences from northeastern Newfoundland. Geographie Physique et Quaternaire, Volume 41, pages 355-364.
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Dyer, A.
1986: A palynological investigation of late Quaternary vegetational history of the Baie Verte Peninsula, northcentral Newfoundland. M.Sc. thesis, Department of Geography, Memorial University of Newfoundland, St. John's, Newfoundland, 182 pages.
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Evans, C.O.
1981: 1980 field report of Frenchmen's Island project. Archaeology in Newfoundland & Labrador 1980, Annual Report 1, pages 88-94.
1982: Frenchmen's Island site (ClAl-1): 1981 preliminary field report. Archaeology in Newfoundland & Labrador 1981, Annual Report 2, pages 210-225.
Fillon, R.H. and Harmes, R.A.
1982: Northern Labrador Shelf glacial chronology and depositional environments. Canadian Journal of Earth Sciences, Volume 19, pages 162-192.
Fitzhugh, W.W.
1972: Environmental archaeology and cultural systems in Hamilton Inlet, Labrador. Smithsonian Contributions to Anthropology, Number 16, 245 pages.
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1975: A Maritime Archaic sequence from Hamilton Inlet, Labrador. Arctic Anthropology, Volume 12, pages 117-138.
1976: Preliminary culture of Nain, Labrador: Smithsonian fieldwork for 1975.
1978a: Maritime Archaic cultures of the central and northern Labrador coast. Arctic Anthropology 15(2), pages 61-95.
1978b: Winter Cove 4 and the Point Revenge occupation of the central Labrador coast. Arctic Anthropology 15(2), pages 146-174.
1980: Preliminary report on the Torngat Archaeological Project. Arctic 33(3), pages 585-606.
1984: Residence pattern development in the Labrador Maritime Archaic: longhouse models and 1983 surveys. Archaeology in Newfoundland & Labrador 1983, Annual Report 4, pages 6-47.
1985a: Early Maritime Archaic settlement studies and central coast surveys. Archaeology in Newfoundland & Labrador 1984, Annual Report 5, pages 48-85.
1985b: The Nulliak pendants and their relation to spiritual traditions in northeast prehistory. Arctic Anthropology 22(2), pages 87-109.
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Lowden, J.A. and Blake, W. Jr.
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Geological Survey Division, Mining and Mineral Development Branch
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