A 550-Year Record of the Disturbance History of White Spruce Forests
Near Two Inuit Settlements in Labrador, Canada
Natasha Roy1,*, Najat Bhiry1, James Woollett2, and Ann Delwaide1
1Centre d’études nordiques and Département de géographie, Université Laval, Québec, G1V 1A0, Canada. 2Centre d’études nordiques and Département des sciences historiques, Université Laval, Québec, G1V 0A6, Canada. *Corresponding Author.
Journal of the North Atlantic, No. 31 (2017)
Abstract
We assessed historical variations in environmental parameters affecting tree growth during the last 550 years in north-central Labrador, Canada, using dendroecological analysis of white spruce forests near two Inuit settlements. Tree surveys of both modern and archaeological wood samples provided data for dendroecological analysis of growth patterns and natural and anthropogenic disturbance regimes and enabled more-refined dendrochronological dating of the occupation of archaeological sites. Previous Quebec-Labrador peninsula dendroecological studies have focused on climatic forcing agents; this study’s coupling of annual tree-growth records to local-scale historical and archaeological data facilitates examination of multi-causal disturbance patterns over time. Low-intensity human interactions with forest ecosystems were significant factors influencing local-scale subarctic forest dynamics in coastal Labrador and should be taken into consideration in other studies.
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A 550-Year Record of the Disturbance History of White Spruce Forests
Near Two Inuit Settlements in Labrador, Canada
Natasha Roy1,*, Najat Bhiry1, James Woollett2, and Ann Delwaide1
Abstract - We assessed historical variations in environmental parameters affecting tree growth during the last 550 years
in north-central Labrador, Canada, using dendroecological analysis of white spruce forests near two Inuit settlements. Tree
surveys of both modern and archaeological wood samples provided data for dendroecological analysis of growth patterns
and natural and anthropogenic disturbance regimes and enabled more-refined dendrochronological dating of the occupation
of archaeological sites. Previous Quebec-Labrador peninsula dendroecological studies have focused on climatic forcing
agents; this study’s coupling of annual tree-growth records to local-scale historical and archaeological data facilitates examination
of multi-causal disturbance patterns over time. Low-intensity human interactions with forest ecosystems were
significant factors influencing local-scale subarctic forest dynamics in coastal Labrador and should be taken into consideration
in other studies.
1 Centre d’études nordiques and Département de géographie, Université Laval, Québec, G1V 1A0, Canada. 2Centre d’études
nordiques and Département des sciences historiques, Université Laval, Québec, G1V 0A6, Canada. *Corresponding Author
- natasha.roy.1@ulaval.ca.
Introduction
Several recent studies have used the association
of variable tree-growth patterns with particular
environmental parameters as a cue for assessing the
large-scale effects of past and present climate on boreal
forest ecosystems (e.g., Caccianiga et al. 2008).
In Labrador, Canada, tree-ring analyses have been
widely used as proxies for climatic conditions such
as temperature and for the teleconnections between
the atmospheric, oceanic, and sea-ice forcings that
structure the climate system (e.g., D’Arrigo et al.
2003, Dickson et al. 1996). Several studies have also
examined climatic influences on Labrador’s forests
at both local and regional scales, indicating that
tree-ring growth records are sufficiently sensitive to
record local effects of large-scale atmospheric variations
such as the North Atlantic Oscillation (NAO)
(e.g., D’Arrigo et al. 2003, Overpeck et al. 1997,
Payette 2007). These studies have demonstrated the
complexity of the relationship between tree growth
and climatic parameters. Very little attention has
been paid, however, to the use of dendroecology to
identify factors influencing tree growth at the local
scale, particularly in relation to forest-disturbance
processes such as insect outbreaks or fires. In the
present study, dendroecological approaches identified
significant forest disturbances in areas having
prolonged Inuit settlement. While these disturbances
appear to be highly localized in the spatial scale,
they nevertheless had measurable impacts on the
evolution of the forest cover as demonstrated by the
frequency of identifiable release events.
Dendroecology measures historical variations in
radial-growth rates to analyze the impact of environmental
changes on tree growth, stand structure,
and stand dynamics (Fritts and Swetnam 1989).
Recently, dendroecology techniques have become
more important for identifying and documenting
historical disturbance regimes in forest stands
(Rubino and McCarthy 2004). As illustrated by
Nowacki and Abrams (1997) and Payette (2010),
tree-rings represent very useful datasets for describing
disturbance regimes, especially long treering
series from forests that have undergone minimal
anthropogenic disturbance.
According to Rubino and McCarthy (2004), a
disturbance represents an event of massive mortality
in a community of living organisms. However,
a disturbance may also be seen as a positive process
mobilizing vital resources (e.g., light, water,
and nutrients) to the benefit of survivors or new
colonizers that leads to local invigoration of growth
(Canham and Marks 1985). Disturbance events may
be endogenous (i.e., pertinent to growth dynamics
of individual stands) or exogenous (i.e., resulting
from factors originating outside the stand) and may
greatly influence radial-growth rates (Cook 1987).
At the regional scale, a disturbance is usually manifested
by the development of canopy-gaps due to
windfall, wood harvesting, fire, insect outbreaks, or
similar events. The presence of a canopy gap induces
a release event, a rapid increase in radial-growth
in nearby trees that had previously been living in
a state of surcimage, i.e., in the absence of light.
Disturbance-history regimes may be reconstructed
by identifying growth-release events manifested in
radial-growth patterns (Nowacki and Abrams 1997,
Payette 2010). These methods provide an objective
2017 Journal of the North Atlantic No. 31:1–14
2017 Journal of the North Atlantic No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
2
representation of past disturbances when release
events are identified according to pre-determined
criteria (mean ring-width, percentage growth rate,
etc.; Rubino and McCarthy 2004).
In order to document anthropogenic forest disturbances
and their impacts in north-central Labrador,
we conducted dendrochronological investigations
in 2 isolated forests surrounded by coastal barrens
in the Nain Bay and Okak Bay regions. These studies
were undertaken in conjunction with ongoing
archaeological research at Inuit winter settlements
(Oakes Bay 1 [HeCg-08] on Dog Island and Uivak
Point [HjCl-09]) within or adjacent to the forestry
study areas (Fig. 1).
Arctic and subarctic environments are stereotypically
considered to be pristine natural environments
lacking anthropogenic disturbances. However, various
aboriginal populations, including Maritime Archaic,
Paleo-Eskimo, and Neo-Eskimo, have called
Labrador home during the last 7000 years. All of
these peoples have transformed, even if only subtly,
the surrounding environment in which they lived by
exploiting the available natural resources. Wood was
one of the most important plant resources in terms of
its diverse and essential roles in daily life (fuel, raw
material, medicine; see Alix 2005) and the volume
in which it was consumed.
Wood has been an essential resource for Inuits,
used as fuel and as raw material for fabricating
material culture essential in everyday life such as
houses, sleds, boats, and tools, both prior to and
following the advent of extensive European contact.
According to Kaplan (2012) and Lemus-Lauzon et
al. (2012), wood use in the Nain region has changed
and adapted to evolving socio-economic conditions
accompanying the expansion of the European colonial
presence in Labrador. Once centers of colonial
exchanges were established in north-central Labrador,
such as the first Moravian mission settlements
in 1771–1783, Inuit resource harvesting became
increasingly oriented towards supplying these European
bases and markets in exchange for trade goods
(Brice-Bennett 1977, Kaplan 1983, Kleivan 1964).
By the 19th century, harvesting wood from forest
stands in the territories around Moravian settlements,
destined for use as fuel and building materials,
became one of the local resources Inuits contributed
in their market exchanges (Kaplan 2012).
Inuit wood harvesting had measurable impacts
in locales distant from European bases as well. For
example, paleo-ecological data published in a recent
study (Roy et al. 2012), revealed that the inhabitants
of the Oakes Bay 1 (HeCg-08) winter village had
considerable impact on the local forest. The discovery
of several cut tree-stumps buried in peat, coupled
with analysis of spruce macrofossils recovered at the
site indicate that, prior to its 17th-century occupation,
the site had a cover of spruce trees (Picea). By
late 20th century, the perimeter of the site was almost
entirely unforested, likely due at least in part to cutting
for building materials and fuel. Today, the site
is an open peat bog with scattered small stands of
spruce and larch, and widespread subfossil spruce
remains preserved in peat. Surrounding the site is an
open spruce forest that contains numerous subfossil
spruce stumps bearing traces of cutting with axes
and saws. Given the long history and broad application
of Inuit wood harvesting in Labrador, it is
necessary to identify the source of disturbances on
isolated forest stands such as those at Oakes Bay .
Methods
Physical setting
This study was conducted in the vicinities surrounding
2 archaeological sites located on Dog
Island and Okak Bay in north-central Labrador
(Fig. 1). The study area lies in the Coastal Barrens
ecoregion of the Labrador coast, which extends
from Napaktok Bay south to the Strait of Belle Isle
(Government of Newfoundland and Labrador 2013).
The majority of the central Labrador coast is characterized
by broad bays and long inlets separated
by prominent capes and headlands and screened by
clusters of islands. Within the sheltered bays, summers
are cool to warm and the growing season is
100 to 120 days (days with temperature over 0°C)
(Government of Canada 2015). Average annual
temperature from 1985 to 2012 was approximately
-2.4 °C and annual precipitation was about 900 mm,
of which about 50% falls as snow (Government of
Canada 2015). The dominant vegetation type is Empetrum
barrens, with black spruce (Picea mariana
[Mill.] Britton et al.) and white spruce (Picea glauca
[Moench] Voss) forests occurring in sheltered valleys.
White spruce established itself in north-central
Labrador ~6000 years ago in the Nain area, by ca.
3000 B.P. in the Dog Island area, and 4500 years
ago in the Okak Bay area, but declined after 2500
B.P. (Lamb 1985, Roy et al. 2012, Short and Nichols
1977). At sites favorable for spruce, trees 100 to 250
years old are common, while trees 250 to 300 years
old may be frequently found in protected and sheltered
areas untouched by insect outbreaks and fire,
such as islands and the Nordic region (Zasada 1984).
Oakes Bay 1 (HeCg-08), Dog Island: Dog Island
is part of the archipelago of Nain Bay (Fig. 1). This
island is located 35 km from Nain, which is currently
the largest Inuit community in Labrador, with 1188
inhabitants (Statistics Canada 2012). The Oakes Bay
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N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
1 archaeological site (HeCg 08), historically known
as Parngnertok (Taylor 1974), is located on a marine
terrace 6 to 8 m above sea level (asl) in a small bay
located on Dog Island’s western shore. Just north
of the site is the steep and cliffy southern slope of
Mount Alagaiai that shelters the bay. The slope from
about 8 to 180 m asl is colonized by an open forest of
white spruce (Fig. 1). According to Zasada (1984),
relatively wet upland conditions such as those of
Oakes Bay are favorable sites for the development
of old-growth spruce forest.
The archaeological site Oakes Bay 1 includes the
ruins of 7 semi-subterranean sod houses of various
sizes. Their floors were dug into sand substrate and
their superstructures were built of stacked blocks of
peat, piled earth, and rock, with wood beams and
posts, as was typical of semi-permanent Inuit sod
houses used in winter (Woollett 2010). According
to the results of archaeological investigations conducted
to date, 2 successive phases of construction
and occupation of sod winter houses can be dated
from late 17th century to early 18th century, and from
mid- to late 18th century (Woollett 2010). Nevertheless,
the immediate locality also has a number of tent
rings and artifact distributions that demonstrate an
ongoing and diverse occupation (apart from the sod
houses themselves) stretching from over 2000 B.P.
to the 20th century. Historical mention of the site’s
sod houses was made in a census taken by Moravian
missionaries during their first winter in the Nain
region (A.D. 1771–1772). This document (summarized
by Taylor 1974, Taylor and Taylor 1977)
reported the use of a single house during that winter,
but made no further note of the use of the sod houses
afterwards, even though subsequent tent camps were
reported in the vicinity. While Oakes Bay 1 seems
to have been abandoned as an intensively occupied
semi-permanent winter village before A.D. 1780,
other winter or year-round settlements were in use
on and around Dog Island throughout the 19th century
and up until the 1970s (Woollett 2003).
Uivak Point (HjCl-9): The archaeological site
of Uivak Point (HjCl-09) is located on the northern
shore of Okak Bay (Fig. 1) about 125 km north of
the village of Nain. The site is 8 km north of the village
of Okak, which was established by Moravian
missionaries in A.D. 1776 and then abandoned in
A.D. 1919 following the catastrophic outbreak of
Spanish flu (Taylor 1974). The dominant vegetation
type surrounding the archaeological site is low arctic
tundra, while white spruce occurs sporadically in
circumscribed groves of 3–10 trees.
The Uivak Point locality has seen repeated occupations
in prehistory and during the recent past.
Several surficial distributions of chipped stone tools
and tent structures found in the vicinity relate to as
yet poorly defined occupations ranging from the
Maritime Archaic (5000 to 3500 B.P.) to Intermediate
Indian populations (3500 to 2000 B.P.), and Pre-
Dorset (3800 to 2200 B.P.) (Cox 1977). Thule/Inuit
used the location on a repeated basis during the 18th,
19th, and 20th centuries (Kaplan and Woollett 2000,
Taylor and Taylor 1977).
The Uivak Point site is a winter settlement comprising
the ruins of 9 semi-subterranean sod houses
constructed on a slope between two boggy terraces
8 and 11 m asl, respectively (Fig. 1). According to
Moravian records, Uivak Point was one of the most
important winter settlements in Labrador during the
late 18th century and the opening years of the 19th
century; it had up to 125 occupants in some years and
was regarded as one of the more successful whaling
communities in Labrador (Kaplan and Woollett 2000,
Taylor 1974, Taylor and Taylor 1977). Archaeological
excavations suggest an initial occupation of
some of the sod houses by the mid-18th century at the
earliest and, according to Taylor and Taylor’s (1977)
synthesis of Moravian census records, the sod-house
site was occupied every winter between 1776 and
1798 and again between 1800 and 1807. No mention
of a subsequent use of the sod houses is reported, although
there were tent camps established there in all
seasons certainly as late as 1829.
Several groups of tent rings of uncertain date but
lacking chipped stone tools distinctive of prehistoric
populations are visible around the locality. As well,
the foundations of 2 more-recent cabin structures
with stone foundations are located on the shore of
the cove adjacent to the sod house site. While the
dates of these houses’ initial occupations are not
known, they were used until 1918 (The survivors …
1986).
Dendroecology analysis
We studied growth patterns of white spruce
stands around Oakes Bay 1 and Uivak Point in a pair
of field sampling surveys conducted in July–August
2010. A total of 154 trees were sampled. From living
trees, 2 cores taken perpendicularly were collected
using a Pressler increment borer at about 25
cm from the root indent collar. Cross-sections were
taken, using a saw, from dead trees at root collar.
At Dog Island, the sampling was carried out near
Oakes Bay, over a 2-km length comprising twenty
10-m-wide transects spaced every 100 m (Fig. 1).
Each individual tree and krummholz (an area of
stunted windblown trees growing at high elevations
on mountain slopes) observed along each 10-m-wide
transect was measured and recorded, but only those
having a diameter greater than 15 cm were sampled
2017 Journal of the North Atlantic No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
4
Figure 1. Location
of the
study sites of
Uivak Point
(upper map)
a n d O a k e s
Bay, Dog Island
(bottom
map). In both
maps, black
l ines show
transect sampling
for the
study.
Journal of the North Atlantic
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N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
in order to have a minimum number of 80 growth
rings in each core. For dead trees, each stump that
could be harvested (i.e., was not buried or decomposed)
was sampled. A total of 133 samples were
recovered, including 41 core samples of living trees
and 92 dead-wood sections. In addition, 4 pieces
of spruce wood exposed during the excavation of
House 2 at the Oakes Bay 1 archaeological site were
collected for analysis.
At Uivak Point, the survey area was defined
following the discovery of old stumps that had
been cut with an axe in a valley 500 m north of the
archaeological site (Fig. 1). Unlike the Dog Island
study area, this region includes only very scattered
solitary trees and small isolated tree stands. Given
the low density of forest cover, all trees that could
be sampled according to the same criterion given
at Oakes Bay were selected, including krummholz.
A total of 15 core samples and 6 dead-wood sections
were taken. Nine spruce trunk specimens were
recovered from sampling trenches excavated in
Houses 6 and 7 in the Uivak Point archaeological
site. A tamarack (Larix laricina [Du Roi] K.Koch)
beam from the roof of the entrance passage of House
6 that had been extracted from permafrost proved to
be sufficiently well-preserved across the breadth of
the trunk to justify dendroecological analysis.
Diagnostic light rings, i.e., growth rings with
exceptionally few latewood cells, were used to date
and cross-date living- and dead-wood sections (Filion
et al. 1986). Archived light-ring chronologies
derived from the L2 tree-ring sequence (1680–1922)
from Okak Bay compiled by Serge Payette and from
Oakes Bay on Dog Island (1620–1978) compiled
by Natasha Roy, available at the Dendrochronology
Laboratory at the Centre for Northern Studies
(CEN), Laval University, were also used as validation
tools. These series allow us to determine the approximate
age of the archaeological wood samples.
Cross-dating was also verified using the program
COFECHA (Grissino-Mayer 2001, Holmes 1983).
Tree-ring widths were measured with a Velmex micrometer
(precision of 0.002 mm) under a binocular
microscope at 40x. We retained only highly intercorrelated
individual curves to build the chronologies of
the Oakes Bay and Uivak Point tree-ring records.
In dendroclimatology, response-function analysis
is used to define the correlation between ring
width and particular climatic variables such as
temperature. Temperature data from the Goose Bay
weather station (Government of Canada 2013) were
used for the calculation of response functions, in
particular mean monthly temperatures during the
current year and the past year from September to
December. Weather data from Goose Bay station
was preferred to data from the nearby Nain stations
since it is more extensive. The CALROB program
from the PPPHALOS package (Guiot 1990) was
used to calculate response functions of white spruce
growth to climatic parameters at Oakes Bay and
Uivak Point. The bootstrap method (Efron 1979,
Guiot 1990) was used for the response functions
based on the repetitive calculation (500 simulations)
of multiple regressions on the same set of climatic
variables. In this study, response functions were calculated
following the methods described by Guiot
and Nicault (2010).
Disturbance-events analysis: In Hudson Bay,
Delwaide and Filion (1987) identified and dated
anthropogenic disturbances such as wood harvesting
in areas occupied by aboriginal peoples using dendroecology
methods. According to Payette (2010),
the relative growth of tree growth rings can be used
to identify and date the presence of canopy-gaps between
trees in a state of surcimage . Growth releases
were detected for individual trees by calculating
the ratio of the width of individual growth rings
relative to those of the 10 preceding and succeeding
years (Berg et al. 2006, Caccianiga et al. 2008,
Nowaki and Abrams, 1997, Payette 2010). A growth
release was defined as a percentage growth change
exceeding 25% over 10 years. Afterwards, the total
growth releases of each tree were arranged in 10-
year classes. Percentage growth change (% GC) was
calculated in yearly increments across individual
tree-ring chronologies. Each % GC value represents
a 20-year span of ring-width data, and empty cells
relative to source tree-ring chronologies occur at
both ends.
Our data showed that growth releases were recorded
as far back as A.D. 1500. However, old-tree
samples (those 300 years old and older) are rare (5
of 154), since many of the old trees were too decomposed
to analyze or were buried. This limitation
may cause an underestimation of disturbance-event
frequency. Consequently, the low number of disturbance
events in the age-characteristic structures of
each site was corrected using log-linear regression
(Morneau and Payette 2000). However, this analysis
assumes a constant decrease in disturbance events
over time. That is why we expressed the fluctuations
in the number of disturbance events by using the
curves of the regression residuals. This approach required
that we add a disturbance event to each of the
age classes for disturbance because of the sporadic
occurrence of years where no events were noted and
the fact that logarithmic transformation is inapplicable
when the value is 0.
2017 Journal of the North Atlantic No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
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We did not have a control site (i.e., a non-disturbed
site), but we observed logged stumps throughout
the area during initial surveys in the study region.
The site studied by Payette et al. (1985) has not
been subject to major natural disturbances and thus
could be regarded as a control site. This site also has
similar ecological characteristics, such as old spruce
trees and the absence of fire disturbance, to the study
sites but is located on the mainland.
Occurrence of insect outbreaks: In northeastern
Canada, the impact of insects on the dynamics of
the forest ecosystem is largely unexplored, and very
little is known about insect outbreaks in Labrador.
Nishimura (2009) has reconstructed the history of
larch sawfly (Pristiphora erichsonii (Hartig)) and
spruce budworm (Choristoneura orae Freeman)
outbreaks in western Labrador but, to our knowledge,
no spruce bark beetle (Dendroctonus rufipennis
Kirby) outbreak has been documented except
for one mentioned by Payette (2007). That outbreak
caused a dieback of white spruce in northern Labrador
between 1989 and 1991. According to Payette
(2007), the spruce bark beetle may also have played
a significant role in the past. For example, in western
North America, massive outbreaks of bark beetles
have infested conifer forests creating extensive
mortality of spruce (Berg et al. 2006). Accordingly,
bark beetle outbreaks represent an important source
of disturbance and must be considered in a study
evaluating anthropogenic impact on forest disturbance.
In this study, spruce bark beetle damage was
assessed by direct observation of white spruce trees,
with a focus on the presence of holes and galleries in
the bark. Previous bark beetle attacks were counted
and dated by recording resin pockets and blue-stain
fungi visible in the wood sections and borer samples.
Resin pockets are crescent-shaped resin accumulations
that can be found either between two annual
rings or within a ring, which is usually deformed
(Caccianiga et al. 2008).
Results
Tree-ring width analyses
The overall forest composition at both sites is
indicative of a rather stable population in terms of
size and structure (Fig. 2). The average age of trees
in the two study areas is 180 ± 55.12 on Dog Island
and 163 ± 61.46 at Uivak Point. Figure 2 shows the
distribution of tree establishment by year. The forest
increased in size after 1780 on Dog Island because
many individual trees appeared after that date. At
Uivak point, the distribution of tree establishment
remained fairly constant over time.
Both woodlands are old-growth stands with trees
of all sizes and ages, including several 300-yearold
white spruce specimens, with the oldest being
384 years old. Spruce mortality (as represented by
sampled dead-wood sections) occurred more or less
throughout the last hundred years in the two study
areas and in particular between 1970 and 2000.
The oldest dead white spruce trees sampled were
established in 1518 and 1666 for the Dog Island and
Uivak Point sites, respectively. The chronologies
extended from A.D. 1518 to 2009 for Dog Island
and from A.D. 1666 to 2009 for Uivak Point. Mean
tree-ring width was similar among the chronologies
(0.312 and 0.263 mm, respectively; Table 1).
The Dog Island white spruce chronology, spanning
A.D. 1518 to 2009, is one of the longest and
oldest presently available in the Nain area, comparable
to those of D’Arrigo et al. (2003) from Salt
Water Pond (AD 1526–1998) and Eyeglass Lake
(AD 1459–1960). It is also, at present, the easternmost
white spruce chronology for North America
and the only one from an island environment.
The response functions of white spruce to climatic
parameters show that tree growth at Dog Island
is positively influenced by July mean temperatures
(Table 2). At Uivak Point, response function analyses
were insignificant. This result is probably due
to the small number of samples at Uivak Point (21
samples) as compared to Dog Island (133 samples).
When the number of samples is small, there is less
chance that the correlation coefficient is high enough
Table 1. Characteristics and statistics of tree-ring series from Dog
Island and Uivak Point.
Parameter Dog Island Uivak Point
Mean ring width (mm) ± SD 0.312 ± 0.12 0.263 ± 0.17
Sensitivity 0.23 0.22
First-year autocorrelation 0.72 0.91
Original time series 1528–2009 1666–2009
Expressed population signal 0.94 -
Table 2. Response functions data set for the mean monthly temperatures during the current growth year and the past year (from September
to December). * indicates significant response functions
Weather
Sites Sept . Oct. Nov. Dec.. Jan. Feb. Mar. Apr. May Jun. Jul. Aug. station
Dog Island -0.442 0.211 1.152 -2.162 -1.548 -0.881 -2.253 -1.181 -0.556 1.210 5.253* 1.244 Goose Bay
Uivak Point -1.353 0.414 1.268 -2.830 -0.483 -0.739 -1.562 -1.356 0.225 1.172 2.306 1.458 Goose Bay
Journal of the North Atlantic
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2017 No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
Figure 2. Distribution over time of tree establishment that composed the forest structure at Dog Island and Uivak Point.
Note that data for the last 100 years are missing due to the sampling methodology (trees smaller than 15 cm diameter were
not sampled).
to confirm a significant correlation with the temperature
data. In general, mean ring widths showed that
tree growth was generally low throughout the period
represented by the chronology (Table 3). However,
the 2 records also indicate that growth rates were
not constant over time and there were short periods
of notable growth. Mean ring widths for 50-year
intervals at Dog Island show that growth rates were
low (below average) during the periods of A.D.
1551–1600 and A.D. 1651–1800 (Table 3). At Uivak
Point, periods of below-average growth were noted
during the 18th and 19th -centuries. Furthermore, at
Table 3. Mean ring width of white spruce for 50-year time periods at Dog Island (DI) and Uivak Point (UP). Mean ring width for Dog Island
is 0.312 ± 0.12 and Uivak Point is 0.263 ± 0.17.
Mean ring width (mm)
1518– 1551– 1601– 1651– 1701– 1751– 1801– 1851– 1901– 1951–
Site 1550 1600 1650 1700 1750 1800 1850 1900 1950 2009
DI 0.320 0.230 0.324 0.265 0.230 0.292 0.308 0.332 0.399 0.548
± 0.17 ± 0.10 ± 0.17 ± 0.12 ± 0.11 ± 0.14 ± 0.16 ± 0.17 ± 0.22 ± 0.33
UP 0.209 0.211 0.216 0.201 0.268 0.413 0.502
± 0.07 ± 0.14 ± 0.12 ± 0.10 ± 0.26 ± 0.30 ± 0.15
2017 Journal of the North Atlantic No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
8
both sites, mean ring widths increased during the
20th century, and the growth rate of younger trees
increased markedly in this century in contrast to
the growth rate of older trees, which was still low.
However, at both sites and throughout the chronologies,
the mean standard deviation of mean ring width
is consistently high, which indicates that values are
widely scattered around the average and that growth
rates of individual trees were not uniform over time.
This finding suggests that neighboring trees had
variable growth-release events in response to forest
disturbances. Moreover, dendrochronological dates
obtained from wood pieces extracted from House
2 at the Oakes Bay site and House 6 at Uivak Point
demonstrate evidence of wood-cutting activities
corresponding to the timing of the these forest disturbances,
although they do not indicate the extent
of wood-harvesting activities (Table 4).
Dendroecology
Growth release. Growth-release episodes occurred
with high frequency at Dog Island and Uivak
Point. At Dog Island, 70% of the trees sampled
showed a minimum of 1 growth release. At Uivak
Point, 62% of trees sampled showed a minimum of 1
growth release. The highest frequency of growth releases
for both sites was recorded at the beginning of
the 20th century (Figs. 3, 4). Prior to that, growth releases
were infrequent, with a small increase around
A.D. 1760 at Dog Island. Between A.D. 1580–1640
and 1690–1760, disturbance events occurred (Fig.
3). Even though their frequency was low, growth
release events extend far back in time to the 16th and
17th centuries (Fig. 3). Such a finding is noteworthy
because it indicates that forest disturbance is an
important process that has influenced forest dynamics
since 1600 AD. In addition, there is a close time
correlation between the positive residual values
and these disturbance events. However, it must be
noted that the first and last 10-year periods of each
chronology must be excluded in the running mean
methodology used in this study.
Long-term reduction in the number of growth
releases with age: Age–frequency distributions of
growth releases at both sites were characterized by
an exponentially decreasing trend over the last 320
and 490 years recorded at Uivak Point and Dog Island,
respectively. According to the residual curve,
it seems that the same trends in the frequency of
growth release over the last centuries apply to both
sites (Figs. 3, 4). In fact, the residual oscillation
around the zero value indicates that the frequency of
growth release increase was sustained.
Resin pockets and blue-stain fungi: Resin
pockets and blue-stain fungi, signs of spruce bark
beetle infestation, were observed at least once in 35
samples from Dog Island, typically from rings dated
after A.D. 1790. Trees on Dog Island show high concentrations
of these marks in A.D. 1800, 1910, and
1920, with a clustered distribution at the end of the
19th century and the beginning of the 20th century. No
resin pockets were found after A.D. 1960. Blue-stain
fungi were observed with the highest frequency between
A.D. 1970 and 2000; dates that also coincide
with a period of significant tree mortality. Most of
the blue-stain fungi were observed in the outermost
part of the wood often associated with holes and galleries
in the bark of recently dead trees. However,
they were also found inside the wood, indicating
that the trees had survived previous bark beetle outbreaks.
Discussion
Using the tree-ring chronologies developed
in this study, we documented forest-disturbance
events that occurred with increasing frequency and
scale over time. These events were inferred from
tree growth releases that occurred when the canopy
opened causing reduced competition for resources
(e.g. light, growing space) and considerably modified
local growth conditions. These disturbance
events appear to be less frequent prior to A.D.
1750 on Dog Island, possibly due to the scarcity of
preserved old trees (which may have been decomposed
or buried). A general increase in disturbance
events was noted on Dog Island between A.D.
1750 and 1800, and disturbance events continued
to have a frequent and consistent impact upon
forest dynamics thereafter. Disturbance events
reached their highest frequency after A.D. 1900
and have remained high since then. The causes of
such events may include climate, fire, insects, and
human activity.
Climate and forest composition and structure
As has been suggested by Berg et al. (2006),
a 10-year mean window for evaluating releases is
long enough to smooth periodicity in ring-widths
associated with the El Nino-La Nina cycle, which
Table 4. Dates from archaeological wood pieces.
Borden
Code Site House ID Species Date
HeCg-08 Dog Island H2 545 Spruce sp. 1634–-1764
HeCg-08 Dog Island H2 OB-1 Spruce sp. 1616–-1741
HeCg-08 Dog Island H2 OB-4 Spruce sp. 1687–-1731
HeCg-08 Dog Island H2 OB-11 Spruce sp. 1618–-1681
HjCl-09 Uivak Point H6 Tamarack 1720–-1825
Journal of the North Atlantic
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2017 No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
Figure 3. Correlation diagram for the last 500 years at Dog Island: (a) occupation periods of the site and surrounding area;
(b) cold climate periods (gray bars) from Meese et al. (1994) and Overpeck et al. (1997); (c) frequency distribution of the
number (nb) of disturbance events (left, bars) and the distribution of the number (nb) of trees by decade (right, line); (d)
frequency distribution of mortality dates; and (e) residuals of the log-linear regression on the age frequency distributions
of release events. In mortality garph, * = dates from archaeological wood pieces..
2017 Journal of the North Atlantic No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
10
Oscillation, whose multidecadal waveform variation
is ~40–60 years (D’Arrigo et al. 2003). δ18O
proxy temperature data from the GISP2 core in
is 3.5 years in Labrador (D’Arrigo et al. 2003). In
addition, a 10-year mean window ought to be short
enough to avoid correlation with the North Atlantic
Figure 4. Correlation diagram for the last 350 years at Uivak Point: (a) occupation periods of the site and surrounding area;
(b) cold climate periods from Meese et al. (1994) and Overpeck et al. (1997); (c) frequency distribution of the number
(nb) of disturbance events (left, bars) and the distribution of the number (nb) of trees by decay (right, line); (d) frequency
distribution of mortality dates; and (e) residuals of the log-linear regression on the age frequency distributions of release
events. In mortality garph, * = date from archaeological wood pieces.
Journal of the North Atlantic
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2017 No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
authors also showed that bark beetle activity, which
had been present along with related blue-stain fungi
since the 18th century, became so widespread in the
20th century that it was linked to extensive waves of
mortality affecting the oldest trees in the 1970s, the
1980s, and especially the 1990s. Similar bark beetle
infestations may also explain the high mortality in
our chronology between 1970 and 2000 when bluestain
fungi were observed in our samples. In order
to distinguish bark beetle disturbance from anthropogenic
disturbance, an entomological study of soil
and peat sediment in the Oakes Bay forest should be
carried out. Such research would make it possible
to determine more precisely when bark beetle outbreaks
occurred (e.g., Bhiry and Filion 1996).
Anthropogenic disturbances
Disturbances resulting from wood harvesting by
humans were documented along the eastern coast of
Hudson Bay at Wapmagoostui-Kuujjuarapik by Delwaide
and Filion (1987). That study illustrated the
significant impact of humans on forest composition
and structure in northern environments. The treering
study presented here demonstrated that release
events have occurred during cold climate periods
as well as during clement ones; in other words, the
release events had little correlation with climatic
trends (Figs. 3, 4). Both of the periods of disturbance
(AD 1500 to 1640 and 1690 to 1750) observed in
the Dog Island samples coincide with periods when
Inuit occupied archaeological sites adjacent to the
study area, most notably the Oakes Bay 1 site. While
dendrochronological analysis could be performed
on only a limited sample of well-preserved archaeological
wood specimens, this analysis was enough
to demonstrate that the site’s occupants probably
harvested wood directly from the studied forest.
Dendrochronological dates (Table 3) combined
with archaeological artifact dates and historical records
related to the occupation of the Oakes Bay 1
site suggest that local tree harvesting may well have
occurred between the years A.D. 1681 and 1771. A
rather longer history of cutting is in fact likely, due
to the presence of other winter settlements and poorly
documented seasonal camps in the locality dating
between the 15th century and the 1970s (Kaplan
1983, Roy et al. 2012, Woollett 2010), all of which
had access to the same forest. The relatively close
clustering of these dates (AD 1681 to 1764) leads
us to conclude that wood present in the Oakes Bay
site was collected from the forest surrounding the archaeological
site. If driftwood had been extensively
used as a building material, a wider dispersion of
tree ages reflective of the more random transport and
Greenland indicate that there were colder climatic
conditions ca, A.D. 1200, 1500, and 1800, whereas
warmer conditions arrived ca. A.D. 1400 and 1700
(Meese et al. 1994). The Labrador tree-ring width
record suggests that there were cooling periods in
the 1600s to early 1700s and in the 1800s, but a
warming period in the middle to late 1700s. Based
on other paleoecological data, a warming trend was
also documented from the late 1800s through the
mid-20th Century (Overpeck et al. 1997). According
to these data, climate does not appear to be a major
cause of the growth releases observed in this study
because the majority of release events are scattered
widely throughout the chronology rather than clustering
around phases of temperature change.
Non-anthropogenic disturbances impact on forest
dynamics
Recent studies of forest dynamics in subarctic
Canada have demonstrated the importance of nonanthropogenic
disturbances such as fire and beetle
outbreak on forest dynamics and tree growth in subarctic
Canada, especially in marginal forest contexts
(Caccianiga et al. 2008). According to Caccianiga et
al., the role of abiotic and biotic disturbances should
not be underestimated. They can have a significant
impact at the local scale on the composition and the
structure of woodland stands and must be considered
in the study of the dynamics of these marginal
forests, especially in the subarctic. We did not find
any clear evidence of fire such as a charcoal layer in
soil or fire scars on trees in the study sites. However,
signs of resin pockets and blue-stain fungi indicate
that bark beetle outbreaks were involved in forest
disturbances in the Dog Island and Uivak Point sites
and likely contributed to a number of release events.
Evidence of bark beetle activity was widespread
at both sites, but the timing and magnitude of each
beetle attack differed. At Uivak Point, only bluestain
fungi were observed, and their distribution was
concentrated between 1980 and 2000, which is in accordance
with Payette (2007). At Dog Island, indices
of bark beetle outbreak were more pronounced. Our
results suggest that the insect has been present for a
long time (since 1790) and that its impact seems to
be greater today. The distribution of resin pockets
and blue-stain fungi shows an important increase in
frequency during the decades following 1800, 1910,
and 1920, and between 1970 and 2000. Similar data
were obtained on the east coast of Hudson Bay by
Caccianiga et al. (2008), who found a high frequency
of occurrence of resin pockets in tree-rings dated
to 1861, 1909, 1914, and 1951 and a high frequency
of blue-stain fungi between 1970 and 1990. These
2017 Journal of the North Atlantic No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
12
to represent the collapsed roof structure of the most
recent phase of construction (and hence occupation)
of that house. It was dated using 4 different unpublished
larch chronologies on file at the Dendrochronology
Laboratory at the Centre d’études nordiques,
Université Laval. All of them indicated a range of
1720–1825, which confirms the best statistical possibilities
for the date. This new information suggests
that 18th- and early 19th-century occupation histories
of some Labrador Inuit sites that were gleaned from
summaries of Moravian Mission records may be
incomplete and need to be verified against independent
archaeological, dendrochronological, or other
pertinent data sources. In this case, artifacts of European
origin recovered in earlier test excavations
of House 6 are consistent with an occupation dated
to A.D. 1825 or shortly thereafter, even though they
are inconclusive (Woollett 2003).A small number of
artifacts recovered in the 2010 excavation, including
wodd pieces, support this interpretation.
At Uivak Point, the frequency of disturbance
events seems less significant than at Dog Island due
to the low number of wood samples analyzed. However,
the data trends in the same direction as the data
from Dog Island. In particular, the frequency of disturbance
events also seems to correspond to the Inuit
occupation period. The beginning of the 20th century
is also marked by high levels of disturbance, which
may be linked to the construction of 2 wood cabins
at the nearby Uivak Point archaeological site in the
late 19th or early 20th century (Woollett 2003).
Conclusion
Reconstructing disturbance regimes by using a
dendroecological approach can provide valuable
data to supplement or substantiate existing information
regarding forest dynamics obtained from other
paleoenvironmental sciences. By coupling data
from this approach to historical and archaeological
data, it becomes possible to document long-term
disturbance patterns, even where previous studies
have concluded that the forest dynamic is primarily
affected by climate. This study demonstrated
that the role of anthropogenic disturbance was very
significant at the local scale in old-growth forests
around the Oakes Bay 1 archaeological site on Dog
Island. Wood-harvesting had a great impact on the
open forest and should be carefully considered in
the study of forest dynamics in the North. Today, the
Oakes Bay forest is sparsely treed and appears to be,
at first glance, a marginal relict forest isolated in a
tundra environment. However, our study of tree-ring
growth in wood sampled from the forest indicates
deposition of flotsam on beaches would likely have
been observed, as has been recently demonstrated
at the Qijurittuq Site (IbGk-3) on Drayton Island,
northern Québec (Lemieux et al. 2011).
The presence of considerable quantities of partially
preserved wood (which was unsuitable for
dendrochronology) throughout the Oakes Bay 1 site
suggests that wood harvesting was a regular and
substantial activity. Plant macrofossil analysis has
also demonstrated anthropogenic impacts (tree cutting)
at the Oakes Bay 1 (Dog Island) site, beginning
sometime after ca. 610 B.P. (AD 1309–1361) and
continuing until ca. 300 B.P. (the late 18th century)
(Roy et al. 2012). This use of the site over the long
term had an impact on local wood resources due to
the extensive amount of wood required to build and
heat their houses (Roy et al. 2012).
This study suggests that episodes of growth release
documented from A.D. 1580 to 1750 coincide
with anthropogenic disturbances in the form of wood
harvesting. Sustained wood harvesting in the relatively
sparse local subarctic forest would have quite
easily generated a significant canopy gap that likely
increased the amount of resources for the remaining
trees, especially light. Light is one of the resources
that is capable of stimulating growth-release events
and is widely associated with disturbance events in
the forest dynamic (Payette 2010).
Disturbance events occurred frequently after
A.D. 1820, with our data showing a maximum disturbance
at the beginning of the 20th century. These
observations suggest that the local forest continued
to be harvested, and new release events continued
to be generated by the presence of new canopy
gaps, well after the Oakes Bay site was abandoned
in the 18th century. This situation can be explained
by the construction of a new winter site ca. A.D.
1820–1830, followed by the construction of wood
cabins in the 20th century at Evilik Bay, located at
the eastern extremity of Dog Island (Fig. 1). Today,
northern Dog Island is still frequented by Inuit for
activities such as wood harvesting, fishing, and berry
picking.
A different scenario of forest disturbance is
portrayed at Uivak Point, however. The A.D.
1720–1825 dates obtained from the wood sample in
House 6 at Uivak Point indicate that the structure
was built and occupied 18 or more years after the
most recent historical mention of the winter village’s
occupation in Taylor and Taylor’s (1977) translation
and synthesis of Moravian mission documents. This
tamarack (eastern larch) specimen was recovered
from a partially frozen deposit overlying the floor of
the entrance passage in House 6. The deposit appears
Journal of the North Atlantic
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2017 No. 31
N. Roy, N. Bhiry, J. Woollett, and A. Delwaide
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that this impression is illusory. Dendrochronological
analyses date Inuit wood harvesting to periods
when the disturbances creating growth releases
were initiated. Therefore, the forest dynamics of
this particular subarctic forest are dominated by a
history of frequent release events that coincide with
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the attendant creation of canopy gaps. Compared to
the effect of human activities, climate change did not
have as great an impact on forest dynamics at this
site.
This case study provides a useful example of the
necessity of adopting a broad frame of reference for
ecological studies in “pristine” contexts where humans
have long histories of occupation. In this case,
a bilateral historical ecology perspective (Crumley
1994) on human environmental interactions provided
a fruitful means of understanding the forest
dynamics and succession of a coastal subarctic
region. The documentation of past disturbance patterns
is primordial for understanding how presentday
forests developed over the recent past and how
they might change in the future.
Acknowledgments
We thank Elie Merkuratsuk and Pier-David Garant
for their assistance in the field. We are also grateful for
the work of the 2010 Uivak field crew and the help of
the Webb family, Tom Sheldon (Director of Environment
for the Nunatsiavut Government), and the community of
Nain. Thanks are also extended to Andrée-Sylvie Carbonneau
for mapping assistance and Richard Vermette for
help with statistical analysis. This project was supported
by grants from the Fonds Québécois de la recherche sur la
société et la culture (FQRSC) supporting the Archeometry
research group of Université Laval, the Fonds Québécois
de la recherche – Nature et Technologie (FQRNT) Doctoral
research scholarships, the Government of Canada
Program for International Polar Year, the Natural Sciences
and Engineering Research Council of Canada (NSERC),
and the Northern Scientific Training Program (Indian and
Northern Affairs Canada).
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