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Relevant bibliographies by topics / Hudson Bay Lowland

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Academic literature on the topic 'Hudson Bay Lowland'

Author: Grafiati

Published: 4 June 2021

Last updated: 15 February 2022

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Journal articles on the topic "Hudson Bay Lowland"

1

Oldham, Michael J., and Samuel R. Brinker. "Additions to the Vascular Flora of Ontario, Canada, from the Sutton Ridges, Hudson Bay Lowland Ecoregion." Canadian Field-Naturalist 125, no. 3 (2011): 241. http://dx.doi.org/10.22621/cfn.v125i3.1227.

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Field studies in the Hudson Bay Lowland ecoregion of northern Ontario during 2010 resulted in the discovery of four native vascular plant species not previously confirmed from the province: Arctic Bellflower (Campanula uniflora; Campanulaceae), Lapland Diapensia (Diapensia lapponica; Diapensiaceae), Alpine Azalea (Kalmia procumbens; Ericaceae), and Alpine Brook Saxifrage (Saxifraga rivularis; Saxifragaceae). These four species are widespread arctic plants occurring in both North America and Eurasia and were found on the Sutton Ridges, a Precambrian bedrock inlier surrounded by the extensive wetlands of the Hudson Bay Lowland.

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Moore, T. R., A. Heyes, and N. T. Roulet. "Methane emissions from wetlands, southern Hudson Bay lowland." Journal of Geophysical Research 99, no. D1 (1994): 1455. http://dx.doi.org/10.1029/93jd02457.

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Klinger, Lee F., and Susan K. Short. "Succession in the Hudson Bay Lowland, Northern Ontario, Canada." Arctic and Alpine Research 28, no. 2 (1996): 172. http://dx.doi.org/10.2307/1551757.

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4

Schiller, C. L., and D. R. Hastie. "Exchange of nitrous oxide within the Hudson Bay lowland." Journal of Geophysical Research 99, no. D1 (1994): 1573. http://dx.doi.org/10.1029/93jd01358.

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5

Larsson, Sven Y., and Colin W. Stearn. "Silurian stratigraphy of the Hudson Bay Lowland in Quebec." Canadian Journal of Earth Sciences 23, no. 3 (1986): 288–99. http://dx.doi.org/10.1139/e86-032.

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Carbonates of late Llandoverian to Ludlovian age, divided into the Severn River, Ekwan River, and Kenogami River formations, crop out in the drainage basin of the Harricana River. The Severn River Formation consists of a succession of alternating wackestone and packstone beds 17.5 m thick. The packstones are ascribed to storm events and carry a deeper water fauna than the wackestones. The Ekwan River Formation is divided into four units: a barren dolostone at the base, sandy wackestones and packstones with a coral fauna, another barren dolomudstone, and at the top a unit of argillaceous, nodular limestone rich in leperditid ostracods. The units are ascribed to shallow subtidal, intertidal, and supratidal environments. Three benthic assemblages, characterized by ostracods, corals, rhynchonellids, and the brachiopods Brachyprion and Dalejina, are distinguished in order of increasing depth. Two transgressive events in Llandoverian C4 and C6 times are marked by coral-rich units in the Severn River and Ekwan River formations.

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6

Westbrook, Cherie J. "Wetlands of the Hudson Bay Lowland: An Ontario Overview." Canadian Water Resources Journal / Revue canadienne des ressources hydriques 39, no. 1 (2014): 83. http://dx.doi.org/10.1080/07011784.2013.872874.

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7

Campbell, D., R. Kwiatkowski, and R. C. McCrea. "Benthic Communities in Five Major Rivers of the Hudson Bay Lowland, Canada." Water Quality Research Journal 21, no. 2 (1986): 235–50. http://dx.doi.org/10.2166/wqrj.1986.018.

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Abstract A total of one hundred and twenty six species of macroinvertebrates were collected from five major Ontario rivers (Moose, Albany, Attawapiskat, Winisk and Severn) of the Hudson Bay Lowland. Benthic communities in all rivers were dominated primarily by chironomids and oligochaetes except in the East channel of the Moose River where gastropods were also a common taxon. Diversity, as measured by both species richness and the Shannon-Weiner index, was not significantly different in each river. Species distribution was related to substrate composition, river velocity and depth at each station. Community similarity analysis showed that rivers geographically closest together, sharing common flow directions and similar drainage basins resembled each other most in terms of benthic communities. The exception to this was the East channel of the Moose River which showed little resemblance to the other Lowland rivers studies. This was attributed to the highly channelized nature of the Moose River and the origin of the East channel itself which is fed by waters draining the Clay Belt, a unique subprovince of the Canadian shield.

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8

Ulanowski, T. A., and B. A. Branfireun. "Small-scale variability in peatland pore-water biogeochemistry, Hudson Bay Lowland, Canada." Science of The Total Environment 454-455 (June 2013): 211–18. http://dx.doi.org/10.1016/j.scitotenv.2013.02.087.

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9

Roulet, Nigel T. "Role of the Hudson Bay lowland as a source of atmospheric methane." Deleted DOIs 99, no. D1 (1994): 1439–54. http://dx.doi.org/10.1029/93jd000261.

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10

Roulet, Nigel T., A. Jano, C. A. Kelly, et al. "Role of the Hudson Bay lowland as a source of atmospheric methane." Journal of Geophysical Research 99, no. D1 (1994): 1439. http://dx.doi.org/10.1029/93jd00261.

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Dissertations / Theses on the topic "Hudson Bay Lowland"

1

Handa, Tanya. "Revegetation trials in degraded coastal marshes of the Hudson Bay lowlands." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape10/PQDD_0003/MQ40695.pdf.

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2

Chang, Esther R. "Seed and vegetation dynamics in undamaged and degraded coastal habitats of the Hudson Bay lowlands." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape2/PQDD_0016/MQ49721.pdf.

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3

Brazeau, Michelle. "Historical Deposition and Microbial Redox Cycling of Mercury in Lake Sediments from the Hudson Bay Lowlands, Ontario, Canada." Thèse, Université d'Ottawa / University of Ottawa, 2012. http://hdl.handle.net/10393/22722.

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The repercussions of climate change are felt worldwide, but Arctic and subarctic regions, where climate warming is expected to be amplified, are especially vulnerable. An episode of mass fish mortality in the Sutton River in the Hudson Bay Lowlands (HBL) of Northern Ontario has elicited the interest of the scientific community. Several lakes were sampled over three years in an effort to better understand and document the changes that may be occurring in these lakes. This study uses sediment cores to assess the history of mercury (Hg) deposition and to assess changes occurring in autochthonous productivity in these lakes. Sediments deposited after the onset of the industrial revolution contained significantly higher concentrations of Hg, with the highest concentrations found in the most recently deposited sediments. Hg concentrations in these pristine lakes rival those of lakes in heavily urbanized areas, indicating that they are in fact subjected to atmospheric deposition of Hg. There was a large variation in [Hg] of the surface sediments of 13 lakes; underscoring the importance of in situ processes in the fate of atmospherically deposited Hg. Methylmercury (MeHg) concentrations were not correlated with total mercury concentrations (THg), demonstrating how THg is a poor predictor of MeHg; the bioaccumulative neurotoxic form of mercury. The S2 fraction of Rock-Eval® Pyrolysis, C:N ratios and ∂13C signatures were used as proxies of autochthonous carbon and all indicated that the lakes have become increasingly productive, presumably due to warmer water temperatures and longer ice-free seasons. Additionally, I use molecular techniques to detect and quantify the merA gene in the sediment; a proxy of bacterial mercury resistance involved in redox transformations. In Aquatuk, Hawley and North Raft Lakes, I observed a subsurface increase in merA genes in the sediment core, independently of a control gene and the [THg]. While I have not been able to explain the driving variables of this subsurface increase, I believe that the role of merA within remote lake sediments deserves further work. Lastly, microcosms were used to measure the production of volatile elemental mercury (Hg(0)) from surface sediments of Aquatuk Lake. I used a combination of analytical and molecular techniques to show that the production of Hg(0) is biogenic and tested the effect of nutrients, pH and ionic strength on the Hg(0) production rates. Ionic strength alone had the greatest impact on Hg(0) production rates, with increased Hg(0) production as ionic strength increases.

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Peterson, Stephen L. "Legacy Effects of Habitat Degradation by Lesser Snow Geese on Ground-Nesting Savannah Sparrows along the Hudson Bay Lowlands." DigitalCommons@USU, 2013. https://digitalcommons.usu.edu/etd/1455.

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Increased growth of the mid-continent population of Lesser Snow Geese (LSGO) has led to the degradation of coastal salt marsh and sedge meadow habitats across Canadian Arctic and sub-Arctic ecosystems. It is believed that a human-induced trophic cascade caused by agricultural habitat modification along migratory routes and wintering grounds has contributed to the increase in LSGO numbers, which has resulted in the alteration of habitat quality and connectivity along northern breeding and stopover sites used by various avian species. This habitat degradation has been shown to decrease the presence and temporal persistence of ground-nesting passerine and shorebird species at a local level and may lead to decreases of Arctic / sub-Arctic breeding avian species across landscapes that LSGO utilize and degrade. In 1999, four paired study plots were established, and used in conjunction with a single study plot from 1976, in order to measure the composition of habitat parameters (barren ground extent; graminoid and shrub cover) and to estimate the number of avian nests found in these plots. Using this historical data along with our findings from 2010 and 2011, our main objectives were to: 1) document the change in the aforementioned habitat parameters over time; 2) estimate the local nesting occupancy rates of the common Savannah Sparrow (SAVS), a robust and adaptable ground nester; and 3) determine which habitat variables are indicative of the rates of change and occurrence of nesting by SAVS within the study plots. By using ANOVA, linear mixed effects, and multi-state occupancy models, results suggest that an increase in barren ground, decreases in shrub and graminoid cover, and a loss of connectivity between suitable nesting patches has led to a 10% (λ = 0.90) annual decline in the probability that SAVS nesting occurred across the study plots from 1999 to 2010. These model results may be used to estimate long-term trends in persistence of breeding SAVS and other similar ground-nesting avian species that share habitats with LSGO along Arctic and sub-Arctic ecosystems. (93 pages)

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Pilon, J. L. "Washahoe Inninou Dahtsuounoaou ecological and cultural adaptation along the Severn River in the Hudson's Bay lowlands of Ontario /." [Ottawa] : Ontario Ministry of Citizenship and Culture, 1987. http://catalog.hathitrust.org/api/volumes/oclc/24303856.html.

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6

Lytwyn, Victor P. "The Hudson Bay Lowland Cree in the fur trade to 1821 : a study in historical geography." 2009. http://hdl.handle.net/1993/3658.

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This is a study of the indigenous people of the Hudson Bay Lowlands, known as the Lowland Cree. The time period is coincident with the European fur trade period in the region from about 1670 to 1821. A review of the archaeological literature has also been included to establish that Aboriginal people occupied the region long before Europeans arrived. The fact that the Lowland Cree lived in the Hudson Bay Lowlands before the arrival of European fur traders is an important element in understanding developments in the post-European contact period. It is also important because it is contrary to the prevailing view in the literature that the resources within the region could not support Aboriginal people without assistance from the European traders. The methodological framework for the study is consistent with traditional approaches in historical geography. A central theme is the relationship between the Lowland Cree and the natural environment. The examination of the human/land interface in the Hudson Bay Lowlands has shown that these people adapted successfully to developments in the fur trade until major transformations to the natural resource base occurred in the late 18th and early 19th century. Contrary to the prevailing view in the literature, most Lowland Cree did not become quickly dependent on the European fur traders. Until the late 18th century many Lowland Cree favoured traditional pursuits over involvement in the commercial trade and wage labour activities. The smallpox epidemic in 1782-83 was a major factor in bringing the Lowland Cree into a more intensive involvement in the fur trade. Contributing to the post-smallpox adaptations among the Lowland Cree was the rapid expansion of the Hudson's Bay Company's inland trading networks. Unusual climatic conditions also played a role in reducing the availability of traditional subsistence and commercial resources. The decline in the caribou population was especially critical in prompting many Lowland Cree to migrate outside of the their traditional homelands. By 1821, the competitive fur trade period had ended throughout much of the Canadian subarctic, and monopoly conditions provided a check against major fur trade developments.

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7

Parrott, Jennifer Alisha. "Multiple Methods for Assessing the Sustainability of Shallow Subarctic Ponds in Churchill Region: Hudson Bay Lowland, Canada." Thesis, 2011. http://hdl.handle.net/10012/6309.

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This thesis examines the occurrence of hydrologic variability in subarctic ponds within the Churchill region of the Hudson Bay Lowland (HBL) and investigates the utility of using remote sensing studies to characterize changes in pond surface area. The thesis also characterizes hydro-climatic change over the past ~60 years, and compares this to pond sustainability within the region of Churchill. A multiple-methods approach incorporating field research, simple water balance modeling and remote sensing is used to address these objectives. Research findings demonstrate the occurrence of natural fluctuations in pond surface area and water levels in the Canadian subarctic. These fluctuations in pond water levels (and thus surface area) are caused by differences in antecedent hydrologic conditions, which are easily detected using remotely sensed imagery and may produce unrepresentative estimates of pond surface area change. Resulting from a 4.5 - 11.8 cm variation in water depth, pond surface areas were significantly altered by antecedent precipitation (average: 3,711 m²), intra-seasonal variability (average: 2,049 m²) and inter-annual climatic variations (average: 1,977 m²). These noteworthy pond boundary and water level differences reinforce the importance of accounting for hydrologic variability when delineating representative pond coverage and sustainability. Contemporary pond sustainability findings reveal significant regional climatic change, changing pond hydrologic conditions and overall pond physical stability between 1947 and 2008. Specifically, the Churchill region has become warmer and wetter. Occurring at a rate of 1.37 mm/yr over the study period, changing atmospheric conditions caused a decrease in open water pond hydrologic deficits. During the hydrologic recharge period, modeled pond water levels exhibited an increasing trend (August +0.72 mm/yr, September 0.51 mm/yr), which suggests ponds are filling closer to their maximum storage capacity prior to freeze-up. A remote sensing analysis of pond boundary modifications in mid-summer revealed no change in contemporary physical pond sustainability. Detected surface area changes from imagery were mainly attributed to naturally induced hydrologic variability. Overall, this thesis suggests a new methodological approach for conducting remote sensing pond sustainability research within the arctic/subarctic environment. As well, this study determined pond sustainability within the Churchill region over the last ~60 years.

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Swystun, Kyle A. "CO2 exchange in a subarctic sedge fen in the Hudson Bay Lowland during two consecutive growing seasons." 2011. http://hdl.handle.net/1993/4509.

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Net ecosystem carbon dioxide exchange (NEE) was measured using the eddy covariance (EC) technique at a wetland tundra-sedge fen near Churchill, Manitoba, Canada during two consecutive growing seasons (2007 and 2008). Mean daily NEE at the fen (DOY 157-254) was -3.5 (± 0.26 S.E.) g CO2 m-2 d-1 in 2007 and -4.6 (± 0.36) g CO2 m-2 d-1 in 2008. The fen was a net carbon dioxide (CO2) sink during both the 2007 and 2008 growing seasons of -343 (± 79) and -450 (± 87) g CO2 m-2, respectively. Mean air temperature during the summer (June 1-August 31) was about 1°C greater than the historical average (1971-2000) in 2007 and about 2°C greater in 2008. Growing season precipitation was 107.5 mm below normal in 2007 and 359.5 mm above normal in 2008. These data suggest that if future climate change brings warmer temperatures and near-to-above average precipitation maintaining the water table near the surface, similar subarctic ecosystems will experience increased gross ecosystem productivity enhancing CO2 sequestration during the growing season.

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9

White, Jerry/Edward. "Characterizing current and past hydroecological conditions in shallow tundra ponds of the Hudson Bay Lowlands." Thesis, 2011. http://hdl.handle.net/10012/6443.

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Due to accelerated climatic warming during the past fifty years, interest and concerns have been growing about changes in the ecological integrity of shallow freshwater ponds that dominate the landscape of the Hudson Bay Lowlands (HBL). Climatic warming is altering the hydrological processes that influence the water balances in these ponds, but knowledge remains insufficient to determine the effects these changes have on ecological conditions in the ponds. To address this knowledge gap, this study examines the relations between current hydrological and limnological conditions and recently deposited sedimentary assemblages of diatoms and photosynthetic pigments in 23 shallow ponds in the HBL. The knowledge from the contemporary studies will be used to inform paleolimnological reconstructions using multiple proxies at two ponds to assess how hydroecological conditions have changed during the past several centuries in response to climatic variations. Water samples were collected three times in 2010 to explore the relations between current hydrological and limnological conditions. The climatic conditions in 2010 provided an excellent opportunity to assess the effects that continued climate warming may exert on hydrolimnological conditions in the study ponds as the warm, dry conditions during the early thaw-season (May- mid-July) followed by extremely wet conditions for the remainder of the thaw-season are likely representative of future climate scenarios. The analysis revealed that the water chemistry in the ponds evolved along one of four different ‘trajectories’ throughout the thaw-season in 2010. These seasonal patterns of limnological conditions closely aligned with similar patterns identified in a study of contemporary hydrological conditions (Light, 2011; Wolfe et al., 2011). The patterns identified in both the hydrological and limnological studies were attributed to differences among ponds in catchment characteristics and hydrological connectivity with adjacent basins. Surface sediment samples were collected in 2010 to determine if hydrolimnological conditions are reflected in the distribution of recently deposited diatom and pigment communities. It was determined that diatom community composition was most highly influenced by the availability of microhabitat in the ponds which did not appear to be controlled by hydrological conditions. Nitrogen availability was determined to be indirectly influencing diatom community composition as the nitrogen-limited conditions in the ponds favoured the proliferation of N2-fixing cyanobacterial mats that provided a large amount of epiphytic habitat in the majority of the study ponds. This resulted in the complete domination of diatom assemblages by one diatom specie that was closely associated with these algal mats in the surface sediments of most ponds. Aphanizophyll, a photosynthetic pigment representative of nitrogen-fixing cyanobacteria, was also in the highest concentration in most of the study ponds as a result of the nitrogen-limiting conditions that allowed these organisms to dominate. Ponds located in the tundra ecozone were also found to have the highest overall pigment concentration which was related to a longer growing season due to the small size of these ponds that resulted in earlier ice-off conditions. The longer growing season of ponds in the tundra ecozone may also be due to high winds that cause a decrease in snow cover, lower surface albedos and an earlier onset of the spring thaw. The paleolimnological reconstruction of two of the ponds revealed similar shifts in diatom community composition in the stratigraphic record even though patterns of past change in their basin hydrology, as explored though the analysis of the δ18OPW record archived in the aquatic cellulose contained in the pond sediments, was very different. The water balance of “Left Lake” was found to be highly influenced by increased evaporation associated with recent warming trends as it is a relatively small basin that becomes hydrologically isolated after the melt period. However, “Erin Lake” was not as susceptible to evaporation during the recent warming trend due to its larger catchment and hydrological connections to other ponds. Both of these ponds experienced marked changes in the diatom assemblages. The changes were characterized by a shift from assemblages containing both small, adnate, benthic taxa that prefer mineral grain substrates and epiphytic taxa that are associated with the cyanobacterial mats covering the pond bottoms to assemblages entirely dominated by epiphytic taxa. The shift in diatom community composition occurred ~1820 in Left Lake, but the timing cannot be determined with any degree of confidence in Erin Lake as no diatoms are observed in the sediment record during the period when the change occurred (~1550 to 1850) due to preservation issues. Analysis of fossil pigments indicates that nitrogen-fixing cyanobacteria have been important to the ecology of the ponds over the entire sediment record. However, there is a trend towards lower concentrations of pigments representative of N2-fixing cyanobacteria in the most recent sediments. The trend in cyanobacterial pigment concentrations coincides with inferred changes in nitrogen availability from the geochemical analysis of the pond sediments by Light (2011). This recent shift in nutrient status may be the result of a number of factors including the increased atmospheric deposition of anthropogenically-derived nitrogen or changes in biogeochemical cycling in the ponds.

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Whittington, Peter. "The Impacts of Diamond Mining to Peatlands in the James Bay Lowlands." Thesis, 2013. http://hdl.handle.net/10012/7352.

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Approximately 7000 to 8000 years ago when Hudson Bay became ice-free the Tyrrell Sea flooded the Hudson basin and deposited fine grained marine sediments overlaying the previous glacial tills. Coincident with the ablation of the ice sheet isostatic rebound occurred causing regression of the Tyrell Sea and the emergence of a flat, relatively impermeable surface that would eventually host one of the world’s largest wetlands: the Hudson Bay Lowlands. The low permeability marine sediments and low regional slope reduced recharge and runoff, respectively, so that basal tidal marshes were established, and with isostatic up lift were eventually replaced by swamp forests and then forested and non-forested bogs. Recent discovery of kimberlite (diamondiferous) pipes in an area of the lowlands has led the development of an open-pit diamond mine which requires dewatering of the regional aquifer. Dewatering is depressurizing the surrounding Silurian bedrock that underlies the marine sediments. It was hypothesized that these marine sediments would act as a confining layer, isolating the overlying peatlands from the regional bedrock aquifer. We tested this hypothesis by instrumenting a 1.5 km long transect located within the zone of the mine’s influence that crossed various bogs and fens overlying these marine sediments, and was anchored at both ends by bedrock outcrops (bioherms), which represented areas of no marine sediment. Along this transect wells and piezometers were installed within the peat profile and upper marine sediments and bedrock to determine changes in water table and hydraulic head. The exposed bedrock outcrops (bioherms) did act as local drainage nodes, however, this effect was limited to ~30 m, beyond which water tables and hydraulic heads were similar to a control site located 25 km away. However, within this 30 m zone daily losses of water by the enhanced recharge often exceeded those of evapotranspiration (~3mm/day) representing a major local loss of water to the system. It is the distance to bedrock, rather than distance to bioherm, that determines strength of recharge. In areas of thinner marine sediments the daily fluxes were similar (but less) than those in the areas directly surrounding the bioherms, despite being 100s of meters away from the bioherms. The stratigraphy surrounding the bioherms lead to complicated flow regimes with higher conductivity layers (e.g., sands) circumventing the lower permeability marine sediments which may help extend the effect of the bioherms beyond the 30 m distance. The drying peat around the bioherms, and the elevated nature of the bioherms in a flat landscape, put them at increased risk for lighting strikes and thus fires; however, very little viable fuel exists in the peatlands around the bioherms and any fires that might occur would be confined to the bioherm and not spread into the surrounding peatland. Overall, at least within the first 5 years of aquifer dewatering, seasonal weather played the dominant role in affecting the hydrology of the peatlands; a heavy snow pack and cool, wet summer can mask, or at least minimize the effects of aquifer dewatering.

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Books on the topic "Hudson Bay Lowland"

1

Riley, J. L. Flora of the Hudson Bay Lowland and its postglacial origins. NRC Research Press, 2003.

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Wilson, Nancy C. Seasonal and geographical distribution of birds for selected sites in Ontario's Hudson Bay Lowland. Ontario Ministry of Natural Resources, 1993.

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Malette, Michael D. Growth and anadromy of brook trout (Salvelinus fontinalis (Mitchill)) from Sutton River, Hudson Bay Lowland. Laurentian University, 1993.

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Jin, Jisuo. Early Silurian brachiopods and biostratigraphy of the Hudson Bay Lowlands, Manitoba, Ontario, and Quebec. Geological Survey of Canada, 1993.

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Jin, Jisuo. Late Ordovician brachiopods and biostratigraphy of the Hudson Bay Lowlands, northern Manitoba and Ontario. Geological Survey of Canada, 1997.

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Wetlands mean life: the Hudson and James Bay lowlands. Environment Canada, 2005.

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Handa, Tanya. Revegetation trials in degraded coastal marshes of the Hudson Bay Lowlands. 1998.

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Chang, Esther R. Seed and vegetation dynamics in undamaged and degraded coastal habitats of the Hudson Bay Lowlands. 2000.

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Pilon, Jean-Luc. Washahoe Inninou Dahtsuounoaou: ecological and cultural adaptation along the Severn River in the Hudson's Bay Lowlands of Ontario. 1986.

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Book chapters on the topic "Hudson Bay Lowland"

1

Martini, I. Peter. "The Hudson Bay Lowland: major geologic features and assets." In Coastal Lowlands. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-017-1064-0_2.

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Dredge, L. A., and L. D. Dyke. "Landscapes and Landforms of the Hudson Bay Lowlands." In World Geomorphological Landscapes. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-35137-3_8.

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Thorleifson, L. H., P. H. Wyatt, W. W. Shilts, and E. Nielsen. "Hudson Bay lowland Quaternary stratigraphy: Evidence for early Wisconsinan glaciation centered in Quebec." In Geological Society of America Special Papers. Geological Society of America, 1992. http://dx.doi.org/10.1130/spe270-p207.

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Martini, I. P. "Chapter 3 The cold-climate peatlands of the Hudson Bay Lowland, Canada: brief overview of recent work." In Developments in Earth Surface Processes. Elsevier, 2006. http://dx.doi.org/10.1016/s0928-2025(06)09003-1.

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Conference papers on the topic "Hudson Bay Lowland"

1

Snyder, Rebecca, Dorothy Peteet, Jonathan Nichols, Sarah Finkelstein, and Maara Packalen. "MACROFOSSIL AND BIOMARKER RECORD FROM HUDSON BAY LOWLAND SOUTH RIDGE HOLLOW BOG, NORTHEAST ONTARIO." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272882.

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Kirkwood, A., P. Roy-Léveillée, M. Packalen, J. McLaughlin, and N. Basiliko. "Evolution of Palsas and Peat Plateaus in the Hudson Bay Lowlands: Permafrost Degradation and the Production of Greenhouse Gases." In 18th International Conference on Cold Regions Engineering and 8th Canadian Permafrost Conference. American Society of Civil Engineers, 2019. http://dx.doi.org/10.1061/9780784482599.069.

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Finkelstein, Sarah A., Kathryn E. Hargan, Kathleen M. Ruhland, et al. "A MULTI-PROXY RECORD OF HOLOCENE PALEOCLIMATE AND PALEOLIMNOLOGICAL CHANGE FROM NORTH RAFT LAKE, HUDSON BAY LOWLANDS, NORTHERN ONTARIO, CANADA." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291091.

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Dalton, April S., Sarah A. Finkelstein, Steven L. Forman, and Peter J. Barnett. "DETERMINING THE AGE OF THE MOST RECENT ICE-FREE INTERVAL IN THE HUDSON BAY LOWLANDS, CANADA, USING OSL DATING: A SIGNIFICANT REDUCTION OF THE LAURENTIDE ICE SHEET DURING THE MID-WISCONSIN GLACIATION?" In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291039.

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Reports on the topic "Hudson Bay Lowland"

1

Jin, J., W. G. E. Caldwell, and B. S. Norford. Late Ordovician brachiopods and biostratigraphy of the Hudson Bay Lowlands, northern Manitoba and Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208903.

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2

Jin, J., W. G. E. Caldwell, and B. S. Norford. Early silurian brachiopods and biostratigraphy of the Hudson Bay lowlands, Manitoba, Ontario, and Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/193322.

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3

Dredge, L. A., and E. Nielsen. Glacial and interglacial deposits in the Hudson Bay lowlands: a summary of sites in Manitoba. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120049.

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