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Dataset: Columbia Financial, Inc. (CLBK) Stock Performance

This dataset provides historical stock market performance data for specific companies. It enables users to analyze and understand the past trends and fluctuations in stock prices over time. This information can be utilized for various purposes such as investment analysis, financial research, and market trend forecasting.

Figure 7 in Mechanism of northern pike invasion in the Columbia River Basin

Figure 7. Heat map showing probability of assignment for 77 individuals sampled from Lake Roosevelt to each population sampled in this study. Potential source populations within the Clark Fork River basin, Coeur d'Alene River basin and recently invaded areas are listed in an upstream to downstream order. While many individuals show an elevated assignment probability to Medicine-Cave Lakes (Coeur d'Alene River basin), 71 of the 77 fish had the highest probability of assignment to populations in the recently invaded waterbodies.

Figure 5 in Mechanism of northern pike invasion in the Columbia River Basin

Figure 5. Heat map showing probability of assignment for 145 individuals sampled from recently invaded areas to potential source populations in the Clark Fork and Coeur d'Alene River basins. Recently invaded areas (y-axis) are listed in upstream (top) to downstream (bottom) order. Source populations within each basin (x-axis) are listed in an upstream (left) to downstream (right) order.

Figure 2 in Mechanism of northern pike invasion in the Columbia River Basin

Figure 2. Sampling locations for northern pike in this study. Grey triangles represent hydroelectric dams that prevent upstream movement of fish. Yellow dots represent northern pike sampling locations.

Figure 4 in Mechanism of northern pike invasion in the Columbia River Basin

Figure 4. Plot of principle coordinates analysis on northern pike genotype data from populations in the Clark Fork River basin (pink dots), Coeur d'Alene-Spokane River basin (yellow dots) and recently invaded areas in eastern Washington (green dots). The percent of variation explained by coordinates 1 and 2 are shown in axes labels.

Figure 6 in Mechanism of northern pike invasion in the Columbia River Basin

Figure 6. STRUCUTRE plot showing population groupings of northern pike captured in recently invaded waterbodies of eastern Washington based on K = 2 populations. Waterbodies are listed in an upstream to downstream order. Nearly all fish captured upstream of Lake Roosevelt belong to one group (red bars). Most individuals captured in Lake Roosevelt belong to a second group (pale green bars), but individuals belonging to the red group are also present in Lake Roosevelt.

Figure 1 in Mechanism of northern pike invasion in the Columbia River Basin

Figure 1. Study area map showing (a) the Columbia River basin and major rivers drainages in this study and (b) waterbodies with populations of northern pike sampled in this study. In (b), black triangles represent hydroelectric dams that prevent upstream movement of fish. Waterbodies in red are primarily located in eastern Washington, USA, and represent the most recently invaded areas.

Figure 3 in Mechanism of northern pike invasion in the Columbia River Basin

Figure 3. Invasion scenarios of northern pike in the Columbia River basin compared using microsatellite data in DIYABC. In all scenarios, the Pend Oreille River was the source of fish in Lake Roosevelt. In Scenario 1 (a), Medicine-Cave Lakes share a common ancestor with Lake Pend Oreille, and Medicine-Cave Lakes were the source of fish to the Pend Oreille River. In Scenario 2 (b), Medicine-Cave Lakes share a common ancestor with Lake Pend Oreille, but Lake Pend Oreille was the source of fish to the Pend Oreille River. In Scenario 3 (c); Medicine-Cave Lakes share a common ancestor and admixture of the two was the source of fish in the Pend Oreille River. In Scenario 4 (d), Lake Pend Oreille shares a common ancestor with an unsampled population. The unsampled population was the source of fish to both Medicine-Cave and the Pend Oreille River. Timelines on the left side of each scenario mark the point of coalescent events; all samples were collected at t0.

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Fig. 3 in A large marine eosauropterygian reptile with affinities to nothosauroid diapsids from the Early Triassic of British Columbia, Canada

Fig. 3. Early Triassic map showing occurrences of Early Triassic (Olenekian) and Middle Triassic (Anisian) with potential apex predators in the respective marine ecosystems. Larger Eosauropterygia are represented by a nothosaur-shape and larger Ichthyopterygia by an ichthyosaur-shape. 1, Nevada and Idaho, USA: ichthyopterygian Thalattoarchon (Anisian), "Cymbospondylus"-like, shastasaur-like ichthyopterygians and Cymbospondylus spp. (Smithian/Spathian–Anisian); 2, British Columbia, Canada: Sauropterygia cf. Nothosauroidea indet. (TMP 1995.116.0023) (Smithian/Spathian–Anisian); 3, Svalbard: "Cymbospondylus" like ichthyopterygians or Pessopteryx? (Smithian/Spathian–Anisian); 4, Central Europe: Cymbospondylus buchseri; Nothosaurus giganteus (Anisian); 5, Luoping, southern China: Nothosaurus zhangi (Anisian). Please note that, although there are Spathian age eosauropterygians and ichthyosaurs known from Anhui Province, eastern China, these are not considered large predators herein, although they could still be apex-predators in their respective ecosystems (compare to Hansen and Galetti 2009). It is further noteworthy that the reptile record from the Smithian is virtually inexistent, with maybe the exception of a few isolated bones (e.g., Massare and Callaway 1994), which so far supports an early rapid dispersal of reptiles mainly during the Spathian. Data and map modified from Scheyer et al. 2014 and Romano et al. 2017, with additions by Fröbisch et al. 2013; Maxwell and Kear 2013; Liu et al. 2014. Abbreviations: Dien., Dienerian; G., Griesbachian; M. Trias., Middle Triassic; Smith., Smithian.

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Fig. 1. 3D in A large marine eosauropterygian reptile with affinities to nothosauroid diapsids from the Early Triassic of British Columbia, Canada

Fig. 1. 3D landscape images of Ganoid Ridge, Wapiti Lake area, British Columbia [downloaded from Google Earth Pro on October 3rd 2018; imagery Landsat/Copernicus (09/14/2011), ©2018 DigitalGlobe, ©2018 Province of British Columbia]. A. Overview of the complete Ganoid Ridge reversed). White letters indicate different cirques at Ganoid Ridge. The stippled white line indicates the trend of the major anticline in the area (adopted from Mutter 2004: fig. 1a and references therein). B. Close-up of the southeastern cirques of Ganoid Ridge seen from the North. The anticline is well visible in the grey sediments of the Permian Mowitch Formation in the E and D cirques, surrounded by the darker brownish colored sediments of the Sulphur Mountain Formation. C. Close-up of the fossil site 54°30'32" N; 120°41'24" W) indicated by the white star in the talus slop of the L cirque, seen from the Northeast. Note that well exposed layers in the E cirque can be traced into the L cirque, indicating a similar stratigraphic succession in both cirques. Abbreviations: MM, Meosin Mountain Member; MO, Mowitch Formation; P, Phroso Member, V, Vega Member.

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Fig. 2. TMP 1995.116.0023 in A large marine eosauropterygian reptile with affinities to nothosauroid diapsids from the Early Triassic of British Columbia, Canada

Fig. 2. TMP 1995.116.0023 tentatively identified as aff. Nothosauroidea indet. from the Olenekian, L cirque locality, Ganoid Ridge, Wapiti Lake area, British Columbia, Canada. The specimen consists of two associated larger slabs (A), and two small slabs (B, C) of unclear association. The area where the preserved bones and imprints on the large slab derive from the skeleton is indicated by a red rectangle on black outline drawing based roughly on Nothosaurus giganteus (based on PIMUZ T 4829). A. The two larger slabs containing most of the identifiable bones. Gastralia, appendicular, and girdle elements are in light gray, axial elements in darker gray. B. Small slab with the imprint of two bone fragments, the larger of which might pertain to a girdle or appendicular bone. C. A second small slab with three partially preserved bone remains, probably all representing adjacent neural arch fragments. Photographs (A1–C1) and interpretative drawings (A2–C2). Abbreviations: c, centrum; ch, hemal arch or chevron bone; g, gastral elements; na, neural arch.

Fig. 8. Recent crustacean Euphausia superba Dana, 1852 in Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada

Fig. 8. Recent crustacean Euphausia superba Dana, 1852 (krill) from Gerlache Strait, Antarctica. A. Left lateral view. B. Dorsal view. C. Detail of stalked eyes after removing head shield. All light micrographs.

Fig. 9 in Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada

Fig. 9. Spiny shields in Recent crustaceans. A. Gnathophausia zoea Willemoes−Suhm 1873 (Malacostraca, Lophogastrida). B. Porcellanid larva (Decapoda). A from http://en.wikipedia.org/wiki/Crustacean; B from www.zooplankton−online.net/gallery.html (courtesy of W.S. Johnson, Goucher College); both used with permission of the copyright holders.

Fig. 5 in Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada

Fig. 5. Bivalved arthropod Isoxys acutangulus (Walcott, 1908), Burgess Shale Formation, middle Cambrian, near Field, British Columbia, Canada (see Fig. 1), general morphology. A. ROM 57902A, headshield in dorsal view without soft parts, note the different angle of the contact between the pleural folds and the cardinal spines, which allows for the position of the stalked eyes. B. ROM 57907A, B; B1, part of unique specimen from WS locality, with eyes, telson and telson flaps; B2, counterpart; B3, line drawing of specimen. C. ROM 57904A; C1, specimen showing paired midgut glands and telson flaps; C2, line drawing of specimen. All dorsoventrally compressed specimens and photographed under polarized light; B2, in water. Midgut glands in gray tone.

Fig. 6 in Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada

Fig. 6. Reconstruction of the bivalved arthropod Isoxys acutangulus (Walcott, 1908), swimming in the water column. Note that the position of the mouth and the attachments of the appendages to the body are conjectural. Not to scale.

Fig. 7. Bivalved arthropod Isoxys longissimus Simonetta and Delle Cave 1975 in Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada

Fig. 7. Bivalved arthropod Isoxys longissimus Simonetta and Delle Cave 1975. Burgess Shale Formation, middle Cambrian, near Field, British Columbia, Canada (see Fig. 1), general morphology. A. USNM 18170, holotype. B. ROM 57910A. C. ROM 57911A. D. ROM 57909A. E. ROM 57908A, B; E1, part of slightly oblique specimen with soft−body preservation, including large eye, telson and some possible exopods; E2, counterpart; E3, line drawing of specimen. F. ROM 57919A. All laterally compressed specimens. A, low angle light from top left; B–F, polarized light.

Fig. 3 in Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada

Fig. 3. Bivalved arthropod Isoxys acutangulus (Walcott, 1908), Raymond Quarry Shale Member, Burgess Shale Formation, middle Cambrian, near Field, British Columbia, Canada (see Fig. 1), general morphology. A. ROM 57898A; A1, specimen showing large stalked eyes and the pair of raptorial frontal appendages; A2, line drawing of specimen. B. ROM 57914A; B1, partially decayed specimen with most of body and appendages rotated towards the front; B2, line drawing of specimen. C. ROM 57899A; C1, specimen with raptorial appendages oriented backwards and possible telson flaps; C2, line drawing of specimen. D. ROM 59871A; D1, considerably decayed specimen showing forward rotation of body and appendage remains; D2, line drawing of specimen. All laterally compressed specimens and polarized light. Midgut glands in gray tone.

Fig. 1. A in Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada

Fig. 1. A. Topographic map of the Burgess Shale area near Field, British Columbia (Canada). The numbers indicate localities where specimens of Isoxys acutangulus (Walcott, 1908) and Isoxys longissimus Simonetta and Delle Cave, 1975 were collected by ROM parties. 1. West slope of Fossil Ridge: 1a, Greater Phyllopod bed, Walcott Quarry; 1b, Raymond Quarry; 1c, "persephone layer" (RQ +20 to +23); 1d, "Tuzoia layer" (TZ); 1e, Collins Quarry—"Ehmaniella Zone" (EZ) and "Upper Ehmaniella" (UE); 2, South face of Mt. Field; 3, North shoulder of Mt. Stephen (ESA, ESB); 4, S7 locality; 5, Mt. Stephen Collins Quarry (WS); 6, Mt. Stephen Trilobite Beds (ST); 7, Stanley Glacier. B. Stratigraphic section of the Burgess Shale and Stephen Formations (modified from Fletcher and Collins, 1998). Circles indicate the levels where specimens of Isoxys acutangulus (Walcott, 1908) and Isoxys longissimus Simonetta and Delle Cave, 1975 from the seven localities in A were collected.

Fig. 4 in Soft-part preservation in two species of the arthropod Isoxys from the middle Cambrian Burgess Shale of British Columbia, Canada

Fig. 4. Bivalved arthropod Isoxys acutangulus (Walcott, 1908), Raymond Quarry Shale Member, Burgess Shale Formation, middle Cambrian, near Field, British Columbia, Canada (see Fig. 1). A. ROM 57905A, B; A1, part of specimen alternating midgut glands, possibly due to compaction, and narrow doublure; A2, specimen under low angle light from top left; A3, counterpart of specimen under low angle light from top left; A4, line drawing of specimen. B. ROM 57906B; B1, specimen with raptorial appendage, and 8 sets of midgut glands; B2, image showing endopod and exopod details; B3, specimen under low angle light from top left; B4, line drawing of specimen. All laterally compressed specimens. A1, B1, B2, polarized light; B2, in water; A2, A3, and B3 dry. Midgut glands in gray tone.