Gerald Osborn's research while affiliated with The University of Calgary and other places
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Publications (78)
We present a new in situ produced cosmogenic beryllium-10 and carbon-14 nuclide chronology from two sets (outer and inner) of alpine glacier
moraines from the Grey Hunter massif of southern Yukon Territory, Canada. The chronology of moraines deposited by alpine glaciers outside the limits
of the Last Glacial Maximum (LGM) ice sheets potentially pro...
Combined use of radiocarbon-dated subfossil wood within lateral moraines and surface exposure ages on moraine boulders provides an approach to better constrain times of glacier advance and onset of retreat. We test this method at Gilbert Glacier in the southern Coast Mountains of British Columbia where units of sediments associated with glacier exp...
The Columbia Icefield is the largest icefield in the Canadian Rockies and feeds eight major glaciers that drain to three different oceans. Previous glacier studies have focused on Athabasca and Saskatchewan Glaciers, primarily due to their easy access. This paper reviews evidence of the Holocene history from all eight glaciers. Maximum Holocene gla...
Some lateral moraines contain a rich record of Holocene glacial expansion. Previous workers have used such evidence to document glacial fluctuations in western Canada, Alaska, and the U.S. Pacific Northwest, but similar studies in Patagonia are uncommon. Here we report on the late Holocene behavior of Stoppani Glacier, a 75 km ² glacier sourced in...
Five large gravitational slope deformation features (GSDFs) in the Lookout Mountain-Tablelands region of western Newfoundland exemplify bedrock slope instabilities in eastern Canada. The Lookout Hills GSDF (8.3 km³) on Bonne Bay (glacial trough) may be the largest GSDF in eastern Canada. It appears to be a post-glacial feature, has vertical total d...
Groundwater flooding can occur when the water table rises due to i) recharge to (or decreased abstraction from) aquifers with low storativity; or ii) propagation of the rising river stages into permeable, river-connected alluvial aquifers. The latter type was significant in 2013 in Alberta. A survey of 189 homes along the Elbow River in Calgary exa...
We analyzed a peat-bog sequence from the central region of Tierra del Fuego, southernmost Patagonia, to reconstruct the environmental changes over the past 15,000 years. Postglacial vegetation was mainly composed by grasslands and shrubby communities with sparsely distributed Nothofagus trees under dry conditions. The predominance of Glomus sp. and...
Lichenometric dating: Science or pseudo-science?—Response to comments by Michael A. O’Neal, pp. 244—245 - Volume 86 Issue 2 - Gerald Osborn, Daniel McCarthy, Aline Walintschek, Randall Burke
A pollen record was obtained from a coring site at La Correntina mire (54º33'S, 66º59'W, 206 m a.s.l.) to the east of Lago Fagnano, centre of Tierra del Fuego. The results indicate that the valley bottom was free of ice shortly before 15,400 cal BP. Pioneer vegetation included dwarf shrub heaths, grasses and herbs with sparsely distributed Nothofag...
The oldest postglacial lapilli–ash tephra recognized in sedimentary records surrounding Mount Rainier (Washington State, USA) is R tephra, a very early Holocene deposit that acts as an important stratigraphic and geochronologic marker bed. This multidisciplinary study incorporates tephrostratigraphy, radiocarbon dating, petrography, and electron mi...
The popular technique of estimating ages of deposits from sizes of lichens continues despite valid criticism, and without agreement on range of utility, treatment of error, and methods of measurement, sampling, and data handling. A major source of error is the assumption that the largest lichen(s) colonized soon after deposition and will survive in...
Most alpine glaciers in the Northern Hemisphere reached their maximum extents of the Holocene between ad 1600 and 1850. Since the late 1800s, however, glaciers have thinned and retreated, mainly because of atmospheric warming. Glacier retreat in western Canada and other regions is exposing subfossil tree stumps, soils and plant detritus that, until...
Most glaciers in western North America with reliable age control
achieved their maximum Holocene extents during final advances of the
Little Ice Age. Tiedemann Glacier, a large alpine glacier in western
Canada, is an enigma because the glacier constructed lateral moraines
that are up to 90 m higher, and extend 1.8 km farther downvalley, than
those...
Castle Creek Glacier in the Cariboo Mountains of British Columbia
remained close to its Little Ice Age limit for most of the past 1500
years, without significant recession until the 20th century. This
conclusion is based on radiocarbon-dated detrital and in-situ plant
material overrun by the glacier, and the sedimentary record from
informally named...
During Holocene advances of the Bear River Glacier, in northwestern British Columbia, ice pushed against a bedrock slope on the north side of Bear River Pass as it was being diverted eastward and westward along the pass. The result is a series of till sheets plastered against the rock slope and separated by wood mats. This sequence of tills provide...
The Holocene and late glacial history of fluctuations of Stutfield Glacier are reconstructed using moraine stratigraphy, tephrochronology, and dendroglaciology. Stratigraphic sections in the lateral moraines contain tills from at least three glacier advances separated by volcanic tephras and paleosols. The oldest, pre-Mazama till is correlated with...
Mount Edziza is a Plio-Pleistocene volcanic complex that is located in the Stikine Terrane in northwestern British Columbia. A sequence of diamictites preserved between Ice Peak Formation basalts on the northwestern blank of Mount Edziza records an Early Pleistocene regional glaciation. The lowest Ice Peak Formation basalt flow (IP1; about 1 Ma) wa...
Ages of glacial deposits in cirques of the Shuswap Highland, British Columbia are approximated or bracketed using tephrochronology, radiocarbon dating and lichenometry. There is evidence for two minor Holocene glacial advances. The younger, named the Raft Mountain Advance, is defined by the type Raft Mountain moraine, which is about 100 years old j...
Bog sediments at an elevation of 1582 m in the upper Elk Valley of British Columbia were dated at three horizons. The lowermost of these, radiocarbon dated at 13 430 ± 450 years BP, provides a minimum age for deglaciation of Elk Valley. This date is probably also a minimum for the Canmore advance in the Bow Valley, Alberta, and suggests that the Ca...
Magnetites of anomalous composition found in association with known Holocene tephras in Banff and Jasper national parks were originally thought to represent a new tephra of unknown origin, but were later associated with Mazama tephra at two other sites in Alberta. New data from Alberta, British Columbia, and Montana confirm the compositional variab...
Waterton Lakes National Park in Alberta and Glacier National Park in Montana lie along adjacent sections of the continental divide in the Rocky Mountains. In cirques or near divides there is evidence for two ages of glacial deposits. Younger deposits are generally well preserved, poorly vegetated, and bear no tephra and no or very small lichens. Ol...
Mazama tephra is a widespread mid-Holocene stratigraphic marker, dating to ca. 6845 BP, and is considered useful for the correlation of Holocene events in western North America. We present evidence from Copper Lake, Alberta, for a tephra layer that underlies Mazama tephra and appears to be a discrete tephra layer but that is indistinguishable from...
A newly discovered molluscan fauna provides an approximate age for a previously undated gravel sequence capping Nose Hill, a relict plateau adjacent to the Bow River in Calgary, Alberta, and constrains the age of the physiographic relief in the area. The fauna consists of a mixed terrestrial–aquatic assemblage whose composition indicates a paleocli...
Most Quaternary research in Canada during the first half of the twentieth century focused on Pleistocene glaciation. Given the dramatic shifts in climate during the Pleistocene, it is not surprising that the Holocene was viewed as a time of benign climate. Holocene climate variability was first recognized around the middle of the century when paleo...
a b s t r a c t We summarize evidence of the latest Pleistocene and Holocene glacier fluctuations in the Canadian Cordillera. Our review focuses primarily on studies completed after 1988, when the first comprehensive review of such evidence was published. The Cordilleran ice sheet reached its maximum extent about 16 ka and then rapidly decayed. Som...
Alpine glacier fluctuations provide important paleoclimate proxies where other records such as ice cores, tree rings, and speleothems are not available. About 20 years have passed since a special issue of Quaternary Science Reviews was published to review the worldwide evidence for Holocene glacier fluctuations. Since that time, numerous sites have...
Sediment cores recovered from alpine and subalpine lakes up to 250 km apart in northern British Columbia contain five previously unrecognized tephras. Two black phonolitic tephras, each 5-10 mm thick, occur within 2-4 cm of each other in basal sediments from seven lakes in the Finlay River - Dease Lake area. The upper and lower Finlay tephras are s...
1] Disparate climate proxies from the Northern Hemisphere record a climate event at 4.2– 3.8 ka. Here we show that glaciers throughout the mountain ranges of western Canada advanced at about this time. This conclusion is based on (1) new and previously reported radiocarbon ages on in situ stumps, logs, branches, and soils exposed by recent retreat...
Sequences of tills, buried paleosols, wood and tephra in lateral moraines provide a record of Holocene advances and retreats of the Bugaboo Glacier in British Columbia. The oldest paleosol is tentatively classified as a Spodosol (Cryorthod). It incorporates Mazama tephra (6,800 B.P.) and charcoal and humus dated at 3,390 and 4.400B.P., respectively...
Holocene glacier fluctuations prior to the `Little Ice Age' in Garibaldi Provincial Park in the British Columbia Coast Mountains were reconstructed from geomorphic mapping and radiocarbon ages on 37 samples of growth-position and detrital wood from glacier forefields. Glaciers in Garibaldi Park were smaller than at present in the early Holocene, al...
The Little Ice Age glacier history in Garibaldi Provincial Park (southern Coast Mountains, British Columbia) was reconstructed using geomorphic mapping, radiocarbon ages on fossil wood in glacier forefields, dendrochronology, and lichenometry. The Little Ice Age began in the 11th century. Glaciers reached their first maximum of the past millennium...
Controversy persists in western Newfoundland regarding Pleistocene, particularly Late Wisconsinan, glacial ice volumes. Independently, a set of alpine glacial deposits on the flanks of the Tablelands in Gros Morne National Park has attracted much attention but little scrutiny. In this study, cosmogenic nuclide dating of the alpine deposits places s...
Evidence from glacier forefields and lakes is used to reconstruct Holocene glacier fluctuations in the Spearhead and Fitzsimmons ranges in southwest British Columbia. Radiocarbon ages on detrital wood and trees killed by advancing ice and changes in sediment delivery to downstream proglacial lakes indicate that glaciers expanded from minimum extent...
The landscape of the Canadian Rockies in southern Alberta is not a direct result of constructional processes; that is, the ridges and peaks have not been pushed into the positions in which we see them today. Tectonic activity provided original elevation but not mountains: at the end of Laramide time, what are now the front ranges and foothills of t...
The sedimentary record of Otokomi Lake, Glacier National Park, Montana, was studied to determine the age of an adjacent Crowfoot moraine. The presence of Mt. St. Helens Jy ash near the bottom of the longest percussion core limits drainage basin deglaciation to before 11 400 14C years before present (BP), although 14 100 BP is the estimated basal ag...
Contrary to popular assumption, the mountainous local relief of the Canadian Rockies probably did not originate with the thrusting that characterized the Laramide Orogeny; rather, that relief is a post-orogenic phenomenon. The magnitude of present local relief in the Rockies thrust-and-fold belt (TFB) depends the relative erosional resistance of ro...
This chapter discusses that the Great Basin (GB) is a region of internal drainage within the Basin and Range Province of the western United States. It is bounded on the west by the Sierra Nevada and Cascade ranges, on the south by the part of the Mojave Desert drained by the Colorado River, on the south and east by the Colorado Plateau, and on the...
We are reconstructing Holocene environments in Garibaldi Provincial Park, in the southern Coast Mountains of British Columbia, by examining a diverse set of paleoenvironmental records, including tree-rings, lake sediments, glacial landforms, and photographs. This integrated study, in combination with previous research in adjacent areas, is providin...
Terrestrial and lake sediment records from several sites in the southern Coast Mountains, British Columbia, provide evidence for an advance of alpine glaciers during the early Holocene. Silty intervals within organic sediments recovered from two proglacial lakes are bracketed by AMS -dated terrestrial macrofossils and Mazama tephra to 8780–6730 and...
Paleoclimate records from northern British Columbia, southwestern Yukon, and adjacent Alaska suggest that Late Holocene climate may have been influenced by specific air mass circulation dynamics. The Aleutian low pressure index (ALPI) is a measure of sea level pressure fluctuations in the Pacific Northwest associated with the Aleutian low (AL) pres...
Sediment cores from Pyramid Lake, an alpine tam in the Cassiar Mountains of northwestern British Columbia, were investigated for changes in pollen, plant macrofossils, charcoal, and clastic sediment, which are used to infer changes in climate throughout the Holocene. Radiometric dating has yielded a chronology of high-magnitude rainstorm events and...
A stratigraphic record from a lake in the Central Plateau Regionof northern British Columbia reveals changes in environment and inferredclimate during the Holocene. Upon deglaciation (ca. 11500 BP), Skinny Lakebecame an embayment of an ice-dammed lake. High clastic sedimentationrates, an unstable landscape, and cool, possibly wet conditions likelyp...
Forty individually named ranges, plateaus, and massifs draining wholly or partly into the Great Basin of the western United States show definite evidence of Pleistocene glaciation. The most obvious deposits are a family of moraines designated, among other names, “Tioga”, “Angel Lake”, and “Pinedale”. Such moraines generally can be traced from range...
Many palaeoenvironmental reconstructions from across western North America indicate that the early to mid-Holocene was warmer and drier than present. The wide distribution of these records suggests that relatively mild and arid conditions were regionally ubiquitous during the early Holocene. In contrast, two recently proposed advances of alpine gla...
The Holocene and late glacial history of fluctuations of Stutfield Glacier are reconstructed using moraine stratigraphy, tephrochronology, and dendroglaciology. Stratigraphic sections in the lateral moraines contain tills from at least three glacier advances separated by volcanic tephras and paleosols. The oldest, pre-Mazama till is correlated with...
A corollary of J. Chlachula's interpretation that chipped quartzite cobbles at the contact of Lake Calgary sediments and underlying till represent an “early Late Wisconsinan” lithics industry is the conclusion that Laurentide and Cordilleran ice did not coalesce in Late Wisconsinan time. Contrary to that conclusion are (1) NW–SE-oriented, streamlin...
The Stikine River Valley (SRV) contains a thick and well-exposed sequence of Late Wisconsinan glaciolacustrine and glacial sediments. The glaciolacustrine sequences record the development of Glacial Lake Stikine (GLS), an advance-phase glacial lake produced when the advance of Coast Mountain glaciers impeded the westward drainage of the Stikine Riv...
In the Canadian and northern American Rockies small-scale fluctuations of glaciers during and after late Wisconsinan deglaciation have been identified using stratigraphy of superimposed glacial deposits, geomorphology, and records of glacial advance in lake and peat sediments.Several authors have proposed that valley-glacier readvances of relativel...
A ca. 9000-yr pollen, macrofossil, and sedimentological record from a laminated sediment core obtained from Susie Lake, British Columbia, reveals changes in vegetation and inferred climate during the Holocene. The pollen record indicates that a shrub and herb assemblage (ca. 9000-7800 yr;BP) was rapidly replaced by a spruce (Picea) and subalpine fi...
In the Stikine River valley, northwestern British Columbia, glacial and nonglacial sediments are preserved beneath Middle Pleistocene basalt-flow remnants that originated from Mount Edziza. The magnetic polarity is consistently normal, indicating that the sediment and the basalts were probably deposited within the Bruhnes normal polarity chron (<78...
There is debate as to whether or not the Younger Dryas (YD) climatic event affected areas outside of the North Atlantic region. The potential of alpine glacial deposits to record the YD is of interest because alpine glaciers would be likely to leave a morainal record even during minor, short-lived advances caused by a period of deteriorating climat...
A suite of sediment core samples was recovered from two lakes, Crowfoot and Bow lakes, that are adjacent to the Crowfoot moraine type locality, to identify and radiocarbon date sediments related to the Crowfoot advance. The Crowfoot moraine system, widely recognized throughout northwestern North America, represents a glacial advance that is post-Wi...
The Little Ice Age was the most extensive Neoglacial glacier advance in the Canadian Rockies. Evidence of earlier, less-extensive Neoglacial glacier advances is based on wood recovered from several glacier forefields. Wood flushed out of Athabasca Glacier (7550-8230 yr B.P., three dates) and Dome Glacier (6120-6380 yr B.P., two dates) indicates tha...
Morphological, chemical, and mineralogical properties of three well-dated buried paleosols within Bugaboo Glacier lateral moraines suggest a complex history of Holocene pedogenesis in which soil development was intermittently interrupted by periods of glacial advance and slope instability. Multiple, buried horizons and cumulic horizons of the paleo...
The notion that much of the earth's erosional flat land has been produced by lateral planation of rivers, held by the late C.H. Crickmay, has been largely ignored in debates over the evolution of landscapes. Evidence is growing, however, that lateral planation is a significant agent in the creation of low-relief landscapes in some regions. Recently...
Although the record of Holocene glacier fluctuations in British Columbia and Alberta is still very fragmentary, much recent progress has been made in their study. Dating of end moraines has been supplemented by studies of lateral moraine stratigraphy and dating of glacially-overridden organic matter upstream of end moraines.Dates from sites close t...
Contemporary glaciers provide a record of relatively small-scale Holocene climatic fluctuations through modern and historical accounts of their advances, retreats, and surges. Reviews some recent work on terminal and lateral moraines, sediments in lakes downstream from glaciers, and regional and global correlation of data on the past 8000 years or...
In the western mountains of the United States and Canada are pre-Neoglacial cirque moraines that lie up to about 3 km outside Neoglacial moraines. There is considerable uncertainty as to the ages of the outer moraines and whether or not they are age-equivalent from range to range. The variety of assigned radiocarbon ages found in the literature may...
Holocene glacial advances in the Banff-Jasper-Yoho area of the Canadian Rocky Mountains have been extremely limited in extent. Limiting 14C dates from two sites within 1 km of contemporary glaciers of fresh terminal moraines indicate that the late Wisconsin Ice Sheet and valley glaciers disappeared prior to 9660 yr B.P. Two subsequent glacial advan...
Citations
... Another way to reconstruct the timing, duration and the scale of glacier retreat in the past is the analysis of organic material primarily of in situ wood (e.g. Agatova et al., 2012;García et al., 2020;Joerin et al., 2008;Le Roy et al., 2015;Luckman et al., 2020;Nicolussi and Patzelt, 2000;Nicolussi and Schlüchter, 2012) and other plant macrofossils (e.g. Humlum et al., 2005;Miller et al., 2017) buried by advancing glaciers and later released due to subsequent glacier retreat. ...
... Evidence for glacier advances remains low until~4.0 cal kyr BP, when records along the western side of the NPI and in the CDI suggest coeval advances around 3.7 cal kyr BP (Bertrand et al., 2012a;Menounos et al., 2020). The latter may have preceded the period of glacier shrinkage recorded by the JPC42 sediment core between 3.9 and 2.4 cal kyr BP (Fig. 8). ...
... Data from this region may therefore provide important information relevant to the present debate about the magnitude, timing, and possible cause(s) of Lateglacial and Holocene glacier and climate variations (e.g. Kutzbach and Guetter, 1986;Davis and Osborn, 1988;Karlé n and Kuylenstierna, 1996). ...
... Based on phototopographic images taken during surveys in 1917 and 1919 these photos provide basic reference materials documenting the historical extent of many of the outlet glaciers from the Icefield (e.g. Luckman, 1988a;Osborn et al., 2001). ...
... As for floods, they are more rapid phenomena in which the role of aquifers is more ambiguous: the buffering effect can consist in storing excess water and mitigating high flows [Chinnasamy, 2016], but Kirchner [2003] highlighted that in many catchments, the flood flows are often mainly composed of groundwater that is mobilised by the excess recharge of aquifers, which was confirmed by local studies [Guérin et al., 2019, Wittenberg et al., 2019. Flood events can even be caused by a rapid increase of water table levels in aquifers, which is known as groundwater flooding [Abboud et al., 2018]. The flood event in the Somme basin in 2000-2001 was concomitant to a rise in the groundwater table of more than 10 m [Pointet et al., 2003], with a large part of flood water carrying the isotopic signature of the chalk aquifer [Négrel and Petelet-Giraud, 2005]. ...
... Alberta despite the increase in interdisciplinary interest in the region as an "ice-free corridor" (Reeves 197 1, 1973;Stalker 1977Stalker , 1978Stalker , 1980Harris and Waters 1977;Jackson 1978Jackson , 1979Jackson , 1980. The additional need for postglacial paleoenvironmental information has also been generated by the interest in the Holocene glacial history of the Canadian Rocky Mountains (Heusser 1956;Gardner 1972;Osborn 1975;Luckman 1977;Harris andHowell 1977, 1978;Luckman et al. 1978;Luckman and Osbom 1979). ...
... Saunders et al. 2018;Xia et al. 2018). There is evidence for a northward shift or expansion of the SHWWduring geomorphology (Mercer 1976;Rabassa & Clapperton 1990;Coronato et al. 2009), pollen (Musotto et al. 2017;Navatini et al. 2019), charcoal analyses (Huber et al. 2004;Mansilla et al. 2016), dendrochronology (Aravena et al. 2002;Masiokas & Villalba 2004) and multiproxy sediment records (Rogers & van Loon 1982;Ariztegui et al. 2007;Moy et al. 2008Moy et al. , 2011Borromei et al. 2010;Lamy et al. 2010;Waldmann et al. 2010;Kilian & Lamy 2012;van Daele et al. 2016;Quade & Kaplan 2017;Zolitschka et al. 2019). These palaeoclimate reconstructions reveal apparently contradictory data and regional syntheses remain controversial (Kilian & Lamy 2012). ...
... This paper largely avoids going over the ground covered by numerous critical reviews [3][4][5][6][7][8][9][10][11][12][13][14]. The intention here is to provide a commentary and background information to help practitioners come to a clearer understanding of the technique and suggest possible future directions. ...
... A wealth of information is available in the literature related to Holocene glacial and paleoclimate change and the readers are referred to Solomnia et al. (2015) for a comprehensive review of the Holocene glacier fluctuations around the globe. On the other hand data on the Holocene glacial record of the Mediterranean region are still relatively scarce compared to LGM record but numerous work have been published in special issues (e.g., Davis and Osborn 1988;Davis et al. 2009;Oliva et al. 2020a, b). ...
... Rainier? Watson et al. (2016) identified a cryptotephra (SV-L5) comprising glass shards of unknown source in Svartkälsjärn, Sweden, mixed with two shards of Hekla origin (possibly Hekla 5/Lairg A) and with an estimated age of~4500-4000 BCE. The unidentified shards include some datapoints whose geochemistries suggest the presence of mineral inclusions in the analyses, but a core group of medium-Ca (CaO~2.5 wt %) composition lies with the geochemical field of proximal glass from Rainier (Sisson and Vallance, 2009;Samolczyk et al., 2016;Fig. 8). ...