Holocene geomorphology and stratigraphy of the lower Falcon valley, Dinosaur Provincial Park, Alberta, Canada

1993 ◽  
Vol 30 (9) ◽  
pp. 1846-1852 ◽  
Author(s):  
Sarah L. O'Hara ◽  
Ian A. Campbell
Keyword(s):  
Great Plains ◽  
Red Deer ◽  
Alluvial Fans ◽  
Lacustrine Deposits ◽  
Southern Alberta ◽  
Recent Phase ◽  
Alluvial Deposition ◽  
Two Phases ◽  
Provincial Park ◽  
Eolian Deposit

A tributary of the Red Deer River in Dinosaur Provincial Park, southern Alberta, contains evidence of a sequence of valley cutting and the deposition of three alluvial fills and one eolian deposit. With the exception of the eolian deposit and minor amounts of Shield and Cordilleran rocks, the sediments are derived from local bedrock. Incision of the bedrock valley occurred in the early postglacial period about 14 000 – 12 000 BP by rapid drainage of proglacial lakes and meltwaters. The valley was subsequently partly infilled as locally fed stream discharges declined during the early to middle Holocene. By 6000–5000 BP alluvial fans had formed along the base of the valley walls. Fan development was followed by two phases of stream entrenchment and alluvial deposition, including the most recent phase of cutting and filling that began approximately 800 BP. The erosional and depositional events may reflect climatic changes as inferred in lacustrine deposits in southern Alberta and in valleys elsewhere in the Great Plains. Glacioisostacy conditions, however, at least in the early Holocene, may have had profound effects on stream base levels.

Red Deer River shakedown: a history of the Captain Marshall field paleontological expedition to Alberta, 1922, and its aftermath

2013 ◽  
Vol 32 (2) ◽  
pp. 204-234 ◽  
Author(s):  
Paul Brinkman
Keyword(s):  
South America ◽  
Late Cretaceous ◽  
Red Deer ◽  
Vertebrate Paleontology ◽  
Fossil Plants ◽  
Southern Alberta ◽  
History Of ◽  
Fossil Vertebrate ◽  
The Moment ◽  
Provincial Park

A Field Museum expedition to collect Late Cretaceous dinosaurs operated for three and a half months in the summer of 1922 in the Red Deer River badlands (Oldman and Dinosaur Park formations, Belly River Group) in an area now known as Dinosaur Provincial Park in southern Alberta, Canada. Associate Curator of Vertebrate Paleontology Elmer S. Riggs led the expedition. He was ably assisted by veteran collectors George F. Sternberg and John B. Abbott. A trio of novice collectors, Anthony Dombrosky, George Bedford and C. Harold Riggs, Elmer's youngest son, rounded out the party. The expedition was a success, netting several quality specimens of duckbilled dinosaurs; one small, partial theropod skeleton; an unidentified duckbilled dinosaur skull; four turtles; other miscellaneous fossil vertebrate remains; numerous fossil plants and invertebrates; and a large fossil log. In 1956, one of these specimens—a nearly complete lambeosaurine hadrosaur reconstructed as Lambeosaurus—debuted as the less fortunate partner of Gorgosaurus in the museum's iconic ‘Dinosaurs, Predator and Prey’ exhibit in Stanley Field Hall. Both of these specimens are still on display in a permanent exhibit called ‘Evolving Planet’. Another notable specimen prepared in 1999-2000 after nearly eighty years in an unopened field jacket has been identified as a juvenile Gorgosaurus. This specimen—nicknamed ‘Elmer’—was recently touring the globe as part of the ‘Dinosaurs: Ancient Fossils, New Discoveries’ exhibit. More importantly, the expedition was an invaluable shakedown experience for the fossil hunting crew and their new equipment in the months before they left on an ambitious, multi-year fossil mammal collecting expedition to Argentina and Bolivia. An oft-repeated myth holds that Riggs viewed the Alberta expedition as a failure and departed the field the moment he obtained permission to go to South America. This paper shows that myth to be unfounded.

Agro-morphology and forage nutritive value of white prairie clover [Dalea candida(Michx.) Willd.] populations native to the Canadian prairies

2018 ◽  
Vol 98 (6) ◽  
pp. 1234-1244
Author(s):  
Nityananda Khanal ◽  
Michael P. Schellenberg ◽  
Bill Biligetu
Keyword(s):  
Great Plains ◽  
Seed Yield ◽  
Nutritive Value ◽  
Block Design ◽  
Northern Great Plains ◽  
Canadian Prairies ◽  
Forage Crop ◽  
Randomized Complete Block Design ◽  
Acid Detergent Fibre ◽  
Provincial Park

White prairie clover [Dalea candida (Michx.) Willd.] is native to the dry prairies and hillsides of the Northern Great Plains. A study was initiated in 2012 with six white prairie clover populations collected from the Canadian Prairies. Plant growth characteristics, forage biomass, seed yield, and forage nutritive values were evaluated using a randomized complete block design in a field near Swift Current, SK. Three populations from Argyle, Carlowrie, and Big Grass Marsh (NCP588) in Manitoba displayed erect-type growth while those from Douglas Provincial Park and Stewart Valley in Saskatchewan and Writing on Stone Provincial Park in Alberta exhibited prostrate growth. The populations did not differ for mean biomass yield (79–104 g plant−1, p = 0.54) and mean seed yield (6.6–9.1 g plant−1, p = 0.69); however, they differed for bloom stage nutritional parameters such as acid detergent fibre (25%–30%, p = 0.04), neutral detergent fibre (34%–41%, p < 0.01), crude proteins (15%–18%, p < 0.01), phosphorus (0.24%–0.29%, p = 0.02), and iron content (144–360 ppm, p = 0.01). To our knowledge, this is the first report of comparative phenotypic, nutritional, and propagation study of native white prairie clover populations of Canada. The constraints and opportunities for successful domestication of white prairie clover as a forage crop are discussed.

High-precision U–Pb CA–ID–TIMS dating and chronostratigraphy of the dinosaur-rich Horseshoe Canyon Formation (Upper Cretaceous, Campanian–Maastrichtian), Red Deer River valley, Alberta, Canada

2020 ◽  
Vol 57 (10) ◽  
pp. 1220-1237 ◽  
Author(s):  
David A. Eberth ◽  
Sandra L. Kamo
Keyword(s):  
High Precision ◽  
Coastal Plain ◽  
Upper Cretaceous ◽  
Red Deer ◽  
Alluvial Plain ◽  
Type Area ◽  
Southern Alberta ◽  
Dinosaur Evolution ◽  
Horseshoe Canyon Formation ◽  
Upper Campanian

The non-marine Horseshoe Canyon Formation (HCFm, southern Alberta) yields taxonomically diverse, late Campanian to middle Maastrichtian dinosaur assemblages that play a central role in documenting dinosaur evolution, paleoecology, and paleobiogeography leading up to the end-Cretaceous extinction. Here, we present high-precision U–Pb CA–ID–TIMS ages and the first calibrated chronostratigraphy for the HCFm using zircon grains from (1) four HCFm bentonites distributed through 129 m of section, (2) one bentonite from the underlying Bearpaw Formation, and (3) a bentonite from the overlying Battle Formation that we dated previously. In its type area, the HCFm ranges in age from 73.1–68.0 Ma. Significant paleoenvironmental and climatic changes are recorded in the formation, including (1) a transition from a warm-and-wet deltaic setting to a cooler, seasonally wet-dry coastal plain at 71.5 Ma, (2) maximum transgression of the Drumheller Marine Tongue at 70.896 ± 0.048 Ma, and (3) transition to a warm-wet alluvial plain at 69.6 Ma. The HCFm’s three mega-herbivore dinosaur assemblage zones track these changes and are calibrated as follows: Edmontosaurus regalis – Pachyrhinosaurus canadensis zone, 73.1–71.5 Ma; Hypacrosaurus altispinus – Saurolophus osborni zone, 71.5–69.6 Ma; and Eotriceratops xerinsularis zone, 69.6–68.2 Ma. The Albertosaurus Bonebed — a monodominant assemblage of tyrannosaurids in the Tolman Member — is assessed an age of 70.1 Ma. The unusual triceratopsin, Eotriceratops xerinsularis, from the Carbon Member, is assessed an age of 68.8 Ma. This chronostratigraphy is useful for refining correlations with dinosaur-bearing upper Campanian–middle Maastrichtian units in Alberta and elsewhere in North America.

Postglacial geomorphic development of the Dinosaur Provincial Park badlands, Alberta

1987 ◽  
Vol 24 (1) ◽  
pp. 135-146 ◽  
Author(s):  
Rorke B. Bryan ◽  
Ian A. Campbell ◽  
Aaron Yair
Keyword(s):  
Red Deer ◽  
Experimental Studies ◽  
Sediment Discharge ◽  
Erosion Rates ◽  
Water And Sediment ◽  
Provincial Park ◽  
Geomorphic Processes ◽  
Aeolian Sands

Experimental studies concerning current geomorphic processes and erosion rates in the badlands of Dinosaur Provincial Park, Alberta, have not explained the unusual extent of badland development or prominent nonstructural near-horizontal surfaces that occur in the park. Two of these surfaces result from spillway development associated with Wisconsin deglaciation, and the extent of badland development is associated with major spillway concentration and exposure of highly erodible Cretaceous strata. A third surface is associated with erosion caused by locally generated runoff. All surfaces are blanketed with aeolian sands and silts deposited around 5500 BP, which profoundly affected the hydrology of the area and water and sediment discharge from the badlands to the Red Deer River. Subsequent stripping of the aeolian cover by streams, along with piping and tunnel erosion, has reexposed vulnerable Cretaceous strata and restored the high erosion rates now observed in these badlands.

ESTABLISHMENT OF ACERIA MALHERBAE (ACARI: ERIOPHYIDAE) AS A BIOLOGICAL CONTROL AGENT FOR FIELD BINDWEED (CONVOLVULACEAE) IN THE NORTHERN GREAT PLAINS

1999 ◽  
Vol 131 (4) ◽  
pp. 541-547 ◽  
Author(s):  
A.S. McClay ◽  
J.L. Littlefield ◽  
J. Kashefi
Keyword(s):  
Biological Control ◽  
Great Plains ◽  
Biological Control Agent ◽  
Control Agent ◽  
Northern Great Plains ◽  
Convolvulus Arvensis ◽  
The North ◽  
Southern Alberta ◽  
Field Bindweed ◽  
Gall Mite

AbstractA European gall mite, Aceria malherbae Nuzzaci, was released and established in southern Alberta and Montana as a biological control agent for field bindweed, Convolvulus arvensis L. (Convolvulaceae). Populations of the mite survived for up to 4 years at some sites and caused slight to severe damage to the weed. The establishment of A. malherbae in these areas suggests that it could be established throughout the North American range of field bindweed.

A Late Mesolithic kill site of aurochs at Jardinga, Netherlands

Antiquity ◽  
2002 ◽  
Vol 76 (292) ◽  
pp. 413-424 ◽  
Author(s):  
Wietske Prummel ◽  
Marcel J.L. Th. Niekus ◽  
Annelou L. van Gijn ◽  
René T.J. Cappers
Keyword(s):  
Red Deer ◽  
Main Phase ◽  
Kill Site ◽  
Two Phases ◽  
A Site ◽  
Late Mesolithic

A site beside the river Tjonger near Jardinga in the northern Netherlands is shown to be a rare Late Mesolithic kill and primary butchering site. Finds consist mainly of bones from aurochs and red deer, with a few flint artefacts. Radiocarbon evidence shows that there must have been two phases of use: the first around 5400 cal BC; the second, main phase around 5250–5050 cal BC.

scholarly journals Radiocarbon Ages of Lacustrine Deposits in Volcanic Sequences of the Lomas Coloradas Area, Socorro Island, Mexico

Radiocarbon ◽  
1993 ◽  
Vol 35 (2) ◽  
pp. 253-262 ◽  
Author(s):  
Jack D. Farmer ◽  
Maria C. Farmer ◽  
Rainer Berger
Keyword(s):  
Volcanic Activity ◽  
Drainage System ◽  
Explosive Volcanism ◽  
Volcanic Hazards ◽  
Lacustrine Deposits ◽  
Socorro Island ◽  
Recent Phase ◽  
Sloping Terrain ◽  
Basaltic Flow ◽  
Historical Accounts

Extensive eruptions of alkalic basalt from low-elevation fissures and vents on the southern flank of the dormant volcano, Cerro Evermann, accompanied the most recent phase of volcanic activity on Socorro Island, and created the Lomas Coloradas, a broad, gently sloping terrain comprising the southern part of the island. We obtained 14C ages of 4690 ± 270 BP (5000–5700 cal BP) and 5040 ± 460 BP (5300–6300 cal BP) from lacustrine deposits that occur within volcanic sequences of the lower Lomas Coloradas. Apparently, the sediments accumulated within a topographic depression between two scoria cones shortly after they formed. The lacustrine environment was destroyed when the cones were breached by headward erosion of adjacent stream drainages. This was followed by the eruption of a thin basaltic flow from fissures near the base of the northernmost cone. The flow moved downslope for a short distance and into the drainages that presently bound the study area on the east and west. The flow postdates development of the present drainage system and may be very recent. Our 14C data, along with historical accounts of volcanic activity over the last century, including submarine eruptions that occurred a few km west of Socorro in early 1993, underscore the high risk for explosive volcanism in this region and the need for a detailed volcanic hazards plan and seismic monitoring.

Late Quaternary landscape evolution and bioclimatic change in the central Great Plains, USA

2020 ◽  
Vol 132 (11-12) ◽  
pp. 2553-2571
Author(s):  
Anthony L. Layzell ◽  
Rolfe D. Mandel
Keyword(s):  
Great Plains ◽  
Landscape Evolution ◽  
Late Quaternary ◽  
Stable Carbon Isotope ◽  
Soil Formation ◽  
River Valley ◽  
Sediment Supply ◽  
Alluvial Fans ◽  
Buried Soils ◽  
South Central

Abstract A systematic study of floodplains, terraces, and alluvial fans in the Republican River valley of south-central Nebraska provided a well-dated, detailed reconstruction of late Quaternary landscape evolution and resolved outstanding issues related to previously proposed Holocene terrace sequences. Stable carbon isotope (δ13C) values determined on soil organic matter from buried soils in alluvial landforms were used to reconstruct the structure of vegetation communities and provided a means to investigate the relationships between bioclimatic change and fluvial activity for the period of record. Our study serves as a model for geomorphological and geoarcheological investigations in stream valleys throughout the central Great Plains and wherever loess-derived late Quaternary alluvial fans occur, in particular. Holocene alluvial landforms in the river valley include a broad floodplain complex (T-0a, T-0b, and T-0c), a single alluvial terrace (T-1), and alluvial fans that mostly grade to the T-1 (AF-1) and T-0c (AF-0c) surfaces. Remnants of a late Pleistocene terrace (T-2), mantled by Holocene (Bignell) loess, are also preserved, and some Holocene alluvial fans (AF-2) grade to T-2 surfaces. Radiocarbon ages suggest that the T-1 fill and AF-1 fans aggraded between ca. 9000–1000 yr B.P. Hence, nearly all of the Holocene alluvium in the river valley is stored in these landforms. Sedimentation, however, was interrupted by several periods of landscape stability and soil formation. Radiocarbon ages from the upper A horizons of buried soils in the T-1 and AF-1 fills, indicating approximate burial ages, cluster at ca. 6500, 4500, 3500, and 1000 yr B.P. Also, based on the radiocarbon ages, the T-0c fill and AF-0c fans were aggrading between ca. 2000–900 yr B.P. Given that the T-0c fill and upper parts of the T-1 fill were both aggrading after ca. 2000 yr B.P., we suggest that the T-1 surface was abandoned between ca. 4500–3500 yr B.P., but subsequent aggradation of both the T-1 and T-0c fills occurred due to large-magnitude flood events during the late Holocene. The δ13C data indicate a shift from ∼40% C4 biomass at ca. 6000 to ∼85% at ca. 4500 yr B.P. We propose a scenario where (1) a reduction in C3 vegetation after 6000 yr B.P. destabilized the uplands, resulting in an increase in sediment supply and aggradation of the T-1 fill and AF-1 fans, and (2) the establishment of C4 vegetation by ca. 4500 yr B.P. stabilized the uplands, resulting in a reduction in sediment supply and subsequent incision and abandonment of the T-1 and most AF-1 surfaces. The proposed timing and nature of landscape and bioclimatic change are consistent with regional records from the central Great Plains.

CANADA'S FIRST KNOWN DINOSAURS: PALAEONTOLOGY AND COLLECTING HISTORY OF UPPER CRETACEOUS VERTEBRATES IN SOUTHERN ALBERTA AND SASKATCHEWAN, 1874–1889

2020 ◽  
Vol 39 (1) ◽  
pp. 184-218
Author(s):  
BRIGID E. CHRISTISON ◽  
DARREN H. TANKE ◽  
JORDAN C. MALLON
Keyword(s):  
Fossil Record ◽  
Upper Cretaceous ◽  
Western Canada ◽  
Vertebral Centra ◽  
Southern Alberta ◽  
The World ◽  
History Of ◽  
British North American ◽  
Diversity Dynamics ◽  
Provincial Park

The early collecting history of dinosaurs and other fossil vertebrates in Western Canada during the 1870s and 1880s is poorly documented. Initial finds were made by the British North American Boundary Commission and the Geological Survey of Canada in modern Saskatchewan and Alberta but, beyond a few well-publicized examples, little is known about precisely what was found and where. Much of the collected material is now housed in the collections of the Canadian Museum of Nature in Gatineau, Quebec, and a recent survey of these historic finds allows for the first comprehensive narrative regarding their identity and procurement. The collection is heavily biased towards vertebral centra and phalanges, reflective of both taphonomic and collecting biases. Given current understanding of Upper Cretaceous assemblages of North America, ornithomimids and small theropods are overrepresented, whereas ceratopsids and ankylosaurs are underrepresented. Fossils from the Belly River Group are best represented, after repeated visits to the areas of present-day Dinosaur Provincial Park and Ross Coulee near Irvine, Alberta. Taxonomic identification of the material has yielded numerous first Canadian occurrences, in addition to some first global occurrences. The latter include the first ever occurrences of Caenagnathidae (1884) and Thescelosauridae (1889). The Upper Cretaceous fossil record of Western Canada is among the richest in the world, and has been thoroughly studied over the last century. These fossils have informed our understanding of dinosaur behaviour, taphonomy, ecology, diversity dynamics, and extinction, among other aspects. But, like the animals themselves, the story of Canada's dinosaur-hunting legacy had humble beginnings—a story that has not been fully revealed before now.

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