INTRODUCTION
The Carbon-14 geochronology date list of
Newfoundland and Labrador provides a complete
catalogue of carbon-14 age dates for the
province. This compilation can be used by
geoscientists for a variety of geological
purposes, including studies in relative sea level
fluctuations, reconstruction of ice margins, and
as a guide for future age-dating work. Readers
are encouraged to examine this document for
accuracy with regard to dates they are familiar
with, and to submit to the authors any other
dates for inclusion. To date, 1339 dates are
included. This compilation will be updated on a
yearly basis as more dates become available.
The data is accessible using web-mapping
software. At present this does not work with all
platforms and browsers- Macintosh users may
experience difficulty. Only Newfoundland dates
are currently mapped. The information can be
found here.
Follow the link to Geoscience
Resources of Newfoundland. If your operating
system and browser are compatible, this will load
the mapping software. By clicking on "surficial
geology" in the lower panel, the radiocarbon
dates will appear as dots overlain on surficial
geology mapping. Full data for each site can be
viewed by clicking on the dots using the
appropriate tool.
In addition the data is available as an Excel file or as
a CSV file (click on these
links and hold down the mouse until you see the
option "download link").
The complete data listing in
html format is also available,
although this is a large table and may take some
time to render on some browsers.
Acknowledgements
Special thanks to Dr. Richard E. Morlan,
Curator of Palaeoenvironmental Studies at the
Canadian Museum of Civilization for permission to
include many of the archaeological dates
contained within this listing.
Explanation of data fields
Reference Number (1:250, 1:50, #)
A reference number has been assigned to
every site location on the map, which comprises
of 3 parts. The first is the 1:250,000 map sheet
on which the age-date occurs (eg., 2M). The
second part is the 1:50,000 map number (eg., 12).
The third part is the reference number assigned
to each sample. These numbers follow
sequentially, beginning at 1 (eg., 2M-12-1). In
cases where there is more than one sample at a
site each sample shares a common reference
number, although they maintain a discrete
laboratory number.
Laboratory Number (Lab #)
This represents the number assigned to
the sample by the laboratory at which it was
dated e.g., GSC-4211. A guide to abbreviations
follows:
- 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 Georiga, USA
- UQ Université de Québec à Montréal
- WAT University of Waterloo
- Y Yale University
Date and Associated Error (Date, Pos, Neg)
The sample date is in years before
present (BP). The age range of these dates is
from modern to greater than 40,000 BP with most
occurring between 1,000 and 14,000 BP. The limit
of carbon-14 dating is currently about 60,000
years; the use of linear accelerators possibly
extend this limit back to about 100,000 years.
All dates have an associated error factor which
results from the random nature of radioactive
decay. The date is therefore given as a time
interval (Pos and Neg) within which the true age
will lie, with a certain probability. Generally,
the error refers to one standard deviation i.e.,
there is a 68% probability that the true age lies
within the time interval given. However, dates
from the GSC are reported within 2 standard
deviations. Furthermore, GSC shell dates are
normalised to d13C=0% PDB, compared to d13C=-25%
PDB for other laboratories. 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).
Locality
Locality refers to the community, lake or
pond closest to where the sample was taken.
Location
The location of the sample site is given
by latitude and longitude, to the closest minute.
Elevation (Elev.)
This generally refers to metres above or
below sea level at which the sample was taken.
For lake sediment samples (e.g., gyttja) lake
surface elevation is given. For dates below sea
level depth is indicated by a minus sign.
Collector (Coll.)
This is the initials of the collector of
the sample. Refer to
Appendix A for names (where known).
Reference
This column represents the source from
which the sample information 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 a
publication, the source is listed in the
reference column. Refer to Appendix B for complete
citations.
Material
Seven different types of materials have
been dated; wood, shells, peat, gyttja (total
organics), whale bone, calcite crystals and
charcoal. The reliability of ages varies between
the types of materials measured, depending on the
amount of carbon present with charcoal and wood
being the most reliable. Other material may be
susceptible to contamination by older or younger
carbon, commonly through the action of
groundwater. This is especially true for total
organic matter samples.
Comments
These are general comments with reference
to the date of the sampled material. In most
cases these are summarized from comments by the
collector.