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Lake Rousseau

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Figure3—Representative teeth of the Lake Rousseau Arctodus simus specimens. UF 223800: 1, R m1; 2, L m2; 3, R m3. UF 223798: 4, L m2. All teeth in occlusal view with anterior towards top of figure.
Published: 01 January 2010
Figure 3 —Representative teeth of the Lake Rousseau Arctodus simus specimens. UF 223800: 1 , R m1; 2 , L m2; 3 , R m3. UF 223798: 4 , L m2. All teeth in occlusal view with anterior towards top of figure.
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Figure4—Arctodus simus ulnae and radius from Lake Rousseau. 1, L ulna, UF 162843; 2, R ulna, UF 162843; 3, L radius, UF 223799. Proximal ends point towards the left of the figure. Scale bars  =  2 cm.
Published: 01 January 2010
Figure 4 — Arctodus simus ulnae and radius from Lake Rousseau. 1 , L ulna, UF 162843; 2 , R ulna, UF 162843; 3 , L radius, UF 223799. Proximal ends point towards the left of the figure. Scale bars  =  2 cm.
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Figure7—Plot of mean REEN concentrations from bones of Rancholabrean (N  =  7) and Hemphillian (N  =  14) mammals from the bed of the Withlacoochee River near Lake Rousseau. Values for Hemphillian mammals are enriched by about two orders of magnitude relative to those from the late Pleistocene and have relatively higher proportions of the lighter REEs such as La, Ce, and Pr. The REE values for UF 223799, radius of Arctodus simus from Lake Rousseau, are significantly different from the Hemphillian sample, and match those of the Rancholabrean sample.
Published: 01 January 2010
Figure 7 —Plot of mean REE N concentrations from bones of Rancholabrean (N  =  7) and Hemphillian (N  =  14) mammals from the bed of the Withlacoochee River near Lake Rousseau. Values for Hemphillian mammals are enriched by about two orders of magnitude relative to those from the late Pleistocene
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Figure5—Bivariate plot of Arctodus pristinus and A. simus m2 dimensions. LR  =  Lake Rousseau specimens; RR  =  Rainbow River specimen. GTDA  =  greatest transverse diameter of anterior half; APD  =  anterior-posterior diameter.
Published: 01 January 2010
Figure 5 —Bivariate plot of Arctodus pristinus and A. simus m2 dimensions. LR  =  Lake Rousseau specimens; RR  =  Rainbow River specimen. GTDA  =  greatest transverse diameter of anterior half; APD  =  anterior-posterior diameter.
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Figure6—Bivariate plot of Arctodus pristinus and A. simus m2 and m3 dimensions. LR  =  Lake Rousseau specimen; RR  =  Rainbow River specimen. GTD  =  greatest transverse diameter; GTDA  =  greatest transverse diameter of anterior half.
Published: 01 January 2010
Figure 6 —Bivariate plot of Arctodus pristinus and A. simus m2 and m3 dimensions. LR  =  Lake Rousseau specimen; RR  =  Rainbow River specimen. GTD  =  greatest transverse diameter; GTDA  =  greatest transverse diameter of anterior half.
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Published: 01 January 2010
Table 3 —Other late Pleistocene mammalian genera and species known from the Rainbow River Arctodus locality (RR 1 ), the entire Rainbow River (RR 2 ), and Lake Rousseau region of the Withlacoochee River (LR). †  =  extinct species. X  =  specimens in UF collection. Identifications by RCH.
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Published: 01 January 2010
Table 2 —Measurements of postcranial Arctodus simus specimens from Lake Rousseau, Florida. Dimensions after von den Driesch (1976) . Observed ranges (OR) for Arctodus pristinus and Arctodus simus from Richards et al., (1996) . X  =  comparative measurements not reported in Richards et al
Journal Article
Published: 01 January 2010
Journal of Paleontology (2010) 84 (1): 79–87.
...Figure 3 —Representative teeth of the Lake Rousseau Arctodus simus specimens. UF 223800: 1 , R m1; 2 , L m2; 3 , R m3. UF 223798: 4 , L m2. All teeth in occlusal view with anterior towards top of figure. ...
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Journal Article
Published: 02 April 2000
Canadian Journal of Earth Sciences (2000) 37 (2-3): 117–133.
..., synchronous with and postdating formation of adjacent volcanic sequences. Ages for the four principal plutons within the complex are: Mistaouac at 2726 ± 2 Ma, Boivin at 2713 ± 2 Ma, Rousseau at 2703 ± 2 Ma, and Paradis at 2686 ± 2 Ma. The latter also constrains deformation within the Laberge deformation zone...
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Generalized geology map with locations of seismic lines used in this compilation and shown in Figs. 2 and 4. Corridor I (referred to in the text) includes reflection line 15 (from AGT92), lines 31, 32, and 33 (from AGT90), and line 71 (Lake Ontario speculation data), as well as refraction – wide-angle reflection lines from the 1992 Abitibi–Grenville refraction – wide-angle reflection experiment (AG92-WAR), and the GRAP-88 experiment. Corridor II comprises the seismic reflection and refraction – wide-angle reflection data from GLIMPCE line J. The geological domain boundaries are from Davidson (1998), the extrapolation of the Grenville Front, Grenville Front Tectonic Zone, CMBbtz southward beneath the Phanerozoic cover are after Forsyth et al. (1994a) and the extrapolation of the Elzevir–Frontenac boundary zone is from Forsyth et al. (1994b). ABT, Allochthon Boundary Thrust; AH, Adirondack Highlands; AL, Adirondack Lowlands; Al, Algonquin domain; Ba, Bancroft terrane; Br, Britt domain; CGB, Central Gneiss Belt; CMB, Central Metasedimentary Belt; CMBbtz, Central Metasedimentary Belt boundary thrust zone; EFBZ, Elzevir–Frontenac boundary zone; El, Elzevir terrane; Fr, Frontenac terrane; GH, Go Home domain; GF, Grenville Front; GFTZ, Grenville Front Tectonic Zone; Ma, Mazinaw terrane; MSZ, Maberly shear zone; Mu, Muskoka domain; PS, Parry Sound domain; PSSZ, Parry Sound shear zone; RLSZ, Robertson Lake shear zone; Ro, Rousseau domain; Sh, Shawanaga domain; SL, Sharbot Lake domain; SSZ, Shawanaga shear zone.
Published: 02 April 2000
, Frontenac terrane; GH, Go Home domain; GF, Grenville Front; GFTZ, Grenville Front Tectonic Zone; Ma, Mazinaw terrane; MSZ, Maberly shear zone; Mu, Muskoka domain; PS, Parry Sound domain; PSSZ, Parry Sound shear zone; RLSZ, Robertson Lake shear zone; Ro, Rousseau domain; Sh, Shawanaga domain; SL, Sharbot
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2006
AAPG Bulletin (2006) 90 (11): 1787–1801.
... et al. (2001) . (B) Generalized lithology and facies characteristics for Midwest Thelma Rousseau 1-12 core in Mecosta County, Michigan (locality 1). Conventional porosity (ruled) and permeability (solid black) measured from the core at every foot is graphically displayed on the right. This facies...
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Journal Article
Published: 05 August 2015
Canadian Journal of Earth Sciences (2015) 52 (8): 537–541.
...-085 . Lewis, L.L. 1978. Stratigraphic palynology of the uppermost Cretaceous and Paleocene formations near Golden, Colorado. M.Sc. thesis, Department of Geology, Colorado School of Mines, Golden, CO. McAndrews , J.H. 2005 . The goosing of Crawford Lake with prehistoric corn pollen...
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Journal Article
Published: 01 February 2018
Canadian Journal of Earth Sciences (2018) 55 (2): 206–220.
.... 2001 . Determination of the drainage structure of a watershed using a digital elevation model and a digital river and lake network . Journal of Hydrology , 374 : 225 – 242 . doi: 10.1016/S0022-1694(00)00342-5 . Turcotte , R. , Rousseau , A. , Fortin , J.-P. , and Villeneuve , J...
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Journal Article
Journal: Geology
Published: 01 July 1998
Geology (1998) 26 (7): 651–654.
...Denis-Didier Rousseau; Richard Preece; Nicole Limondin-Lozouet Abstract We present a high-resolution record from a late glacial–Holocene land-snail succession from southeast England. Temperature estimates, derived from the best analogue technique, indicate a cooling trend, between 14 500 and 12 600...
Journal Article
Journal: Geosphere
Published: 19 January 2021
Geosphere (2021) 17 (2): 455–478.
... (i.e., north of latitude 39°N) are widely dispersed, exposing range-parallel belts of deformed and metamorphosed country rock of both continental and oceanic affinity that compose the metamorphic belts of the Sierra Nevada foothills ( Saleeby et al., 1989a ; Cecil et al., 2012 ; Rousseau, 2016...
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Journal Article
Published: 02 May 2018
Canadian Journal of Earth Sciences (2018) 55 (8): 958–979.
...–Cu–Co–PGE Ferguson Lake deposit is hosted by >2.6 Ga hornblenditic to gabbroic rocks of the Ferguson Lake Igneous Complex (FLIC), which is metamorphosed up to amphibolitic facies. The FLIC has a basaltic composition (Mg# = 31–72), flat to slightly negatively sloped normalized trace element...
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Journal Article
Journal: Geology
Published: 01 October 2004
Geology (2004) 32 (10): 885–888.
...John W. Magee; Gifford H. Miller; Nigel A. Spooner; Daniele Questiaux Abstract Our reconstructed history of Lake Eyre provides the first continuous continental proxy record of Australian monsoon intensity over the past 150 k.y. This continental record's broad correspondence to the marine isotope...
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Journal Article
Published: 01 April 2007
Mineralogical Magazine (2007) 71 (2): 235–240.
... and Rousseau (2003) described the variations observed in this double salt composition, in the sulphate (S), burkeite (B) and carbonate (C) regions as a function of solution composition, at an experimental temperature of 115°C. They found that most of the data in the burkeite region indicate that sodium...
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Journal Article
Published: 14 February 2024
Canadian Journal of Earth Sciences (2024) 61 (3): 286–295.
... clusters ranging up to large sites of 100–200 dwellings in areas with good access to anadromous fisheries; this has been named the Plateau Pithouse Tradition ( Richards and Rousseau 1987 ). The number and size of pithouses reached an apogee during the Classic Lillooet Phase, just prior to ∼1.1 ka ago...
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Journal Article
Published: 01 May 2008
Vadose Zone Journal (2008) 7 (2): 830–842.
...-A 262, 2006 ) or simple first-order decay models (e.g., Kadlec and Knight, 1996 ; Rousseau et al., 2004 ). However, Kadlec (2000) documents that first-order models are inadequate for the design of treatment wetlands. Werner and Kadlec (2000 ) modeled the nonideal flow of CWs with a network...
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