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Fig. 1. NGHP-01 in A new neolepadid cirripede from a Pleistocene cold seep, Krishna-Godavari Basin, offshore India
Fig. 1. NGHP-01 core sites (circles) and logging sites (stars) in the offshore Krishna-Godavari Basin, modified from Lorenson and Collett (2018). Site 12 is co-located with sites 10 and 21 (red circle). Inset shows the study area in Krishna-Godavari Basin is located on the eastern margin of peninsular India in the western Bay of Bengal.
Fig. 1 in Lamellorthoceratid cephalopods in the cold waters of southwestern Gondwana: Evidences from the Lower Devonian of Argentina
Fig. 1. Location map of the studied fossil localities and middle Palaeozoic outcrops (A, B) and stratigraphic sections with fossil occurrences indicated (C).
Fig. 2 in Lamellorthoceratid cephalopods in the cold waters of southwestern Gondwana: Evidences from the Lower Devonian of Argentina
Fig. 2. Lamellorthoceratid cephalopod Arthrophyllum sp. from the Lower Devonian Talacasto Formation in the Precordillera Basin, Argentina. A. CEGHUNC 27426, general view of the longitudinal section of the specimen (A1), details showing a closer view of the lamellae and siphuncle structure (A2–A5), external view (A6), specimen before cutting in posterior view (A7). Note the lamellar deposits where the septum is removed. B. CEGH-UNC 27427, specimen in lateral view (B1), posterior views with different orientations (B2, B3). C. CEGH-UNC 27428, lateral views of the internal mould with different orientations (C1–C3), internal mould in posterior view (C4), external mould in anterior view, showing the lamellar deposits inside the apicalmost chamber (C5), external mould in lateral view with the same lamellar deposits in the posterior part (C6). Scale bars 5 mm.
Fig. 3 in Ecology Of The Cold-Adapted Species Nebria Germari (Coleoptera: Carabidae): The Role Of Supraglacial Stony Debris As Refugium During The Current Interglacial Period
Fig. 3. Sampling data are expressed as average Activity Density (AD: number of individuals per day of trap activity). Whiskers represent standard deviation
Fig. 1 in Ecology Of The Cold-Adapted Species Nebria Germari (Coleoptera: Carabidae): The Role Of Supraglacial Stony Debris As Refugium During The Current Interglacial Period
Fig. 1. Map with the position of the two sampling sites (Agola and Sorapiss). At the top left, a picture of N. germari taken on Sorapiss. (Photo by D. Dalpiaz and F. Pupin/ Archive MUSE)
Figure 1 in Avoidance of cold-, cool-, and warm-water fishes to Zequanox exposure
Figure 1. Overhead schematic of the avoidance system. Source water entered from the left and flow rates were controlled with diaphragm valves and monitored on side-specific rotameters. A cross-over system included a set of 3-way valves and plumbing to switch treatment sides during trials. Flow collimators of decreasing sizes on both sides of the choice tank delivered near laminar flow conditions to the arena. Fish were contained in the arena by the collimator upstream and by a backscreen on the downstream side. The samplers included a pH probe, dissolved oxygen probe, and peristaltic tubing to monitor test conditions from outside the curtain without disturbing the test individual.
Figure 3 in Avoidance of cold-, cool-, and warm-water fishes to Zequanox exposure
Figure 3. Comparison of behavior effect sizes and confidence intervals by species assessing the response to Zequanox exposure in a two-flume choice tank. Species are Fathead Minnow (FHM), Bluegill (BLG), Yellow Perch (YEP), Lake Sturgeon (LST), Lake Trout (LAT), and Brook Trout (BKT). Diamonds represent the species' mean behavior effect sizes and the error bars represent the 95% confidence interval. Negative values for the behavior effect sizes are considered an attraction response and positive values are considered an avoidance response.
Figure 2. Representative trial format for showing side B in Avoidance of cold-, cool-, and warm-water fishes to Zequanox exposure
Figure 2. Representative trial format for showing side B (above centerline) treated first. Zequanox concentrations in mg/L as active ingredient (shaded area) for each side of the choice tank. One trial per species (n = 6) was sampled every 5 minutes during the control period and every 2 minutes thereafter. The control period was preceded by a 10-minute acclimation period.
Supplementary Data for: Worldwide consequences of a mid-Holocene cold event in the Nordic Seas
<p>SupplementaryTable1.xlsx lists all the samples used to calculate the regional reservoir correction.</p> <p>SupplementaryTable2.xlsx lists all information on the individual radiocarbon dates of all the cores used in the study: LabID, Depth [cm], 14C age ± error, Calibrated age (95% confidence range and mean), and Dated species. Please note that the age-depth relationships have been modeled using a Bayesian approach so the Calibrated ages might differ from the ages that would be yielded by the calibration of individual radiocarbon ages.</p> <p>SupplementaryTable3.xlsx contains all the data used in the study:</p> <p>OCE2017-GR02:<br>- Depth [cm] <br>- Age [ka BP] (this study)<br>- <em>N. pachyderma </em>[%] (Telesiński et al. 2022)<br>- summer sSST 100m [°C] (this study)</p> <p>MSM5-5-723:<br>- Depth [cm]<br>- Age [ka BP] (this study)<br>- <em>N. pachyderma</em> [%] (Werner et al. 2015)<br>- summer sSST 100m [°C] (this study)<br>- P<sub>B</sub>IP<sub>25</sub> (Werner et al. 2015)<br>- Planktic foraminifera fragmentation [%] (Werner et al. 2003)</p> <p>JM10-330GC:<br>- Depth [cm]<br>- Age [ka BP] (this study)<br>- <em>N. pachyderma </em>[%] (Consolaro et al. 2018)<br>- summer sSST 100m [°C] (this study)<br>- Planktic foraminifera [ind./g] (Consolaro et al. 2018)</p> <p>MSM5-5-712:<br>- Depth [cm]<br>- Age [ka BP] (this study)<br>- <em>N. pachyderma </em>[%] (Werner et al. 2013)<br>- summer sSST 100m [°C] (this study)<br>- IRD flux [#/cm**2/kyr] (Werner et al. 2013, recalculated to the new age model)<br>- P<sub>B</sub>IP<sub>25 </sub>(Müller et al. 2012)</p> <p>M23258:<br>- Depth [cm]<br>- Age [ka BP] (this study)<br>- <em>N. pachyderma </em>[%] (Sarnthein et al. 2003)<br>- summer sSST 100m [°C] (this study)<br>- annual SST [°C] (Martrat et al. 2003)</p> <p>M17730-4<br>- Depth [cm]<br>- Age [ka BP] (this study)<br>- <em>N. pachyderma </em>[%] (Telesiński et al. 2015)<br>- summer sSST 100m [°C] (this study)<br>- Planktic foraminifera [ind./g] (Telesiński et al. 2015)</p> <p>MD95-2011<br>- Depth [cm]<br>- Age [ka BP] (this study)<br>- <em>N. pachyderma </em>[%] (Risebrobakken et al. 2003)<br>- summer sSST 100m [°C] (this study)<br>- Planktic foraminifera [ind./g] (Risebrobakken et al. 2003)</p> <p>MD99-2284<br>- Depth [cm]<br>- Age [ka BP] (this study)<br>- <em>N. pachyderma </em>[%] (Bakke et al. 2009, Eldevik et al. 2014)<br>- summer sSST 100m [°C] (this study)</p> <p>JM09-020<br>- Depth [cm]<br>- Age [ka BP] (this study)<br>- annual SST [°C] (Łącka et al. 2019)</p> <p>SupplementaryFigure1.pdf shows Age-depth relationships of cores used in the study as modeled using a Bayesian approach with the Bacon software (Blaauw and Christen, 2011). Dark shading indicates the more likely ages for a given depth, the grey dashed line indicates the 95% confidence range, and the red dashed line indicates the best-fit (mean) age model.</p> <p>SupplementaryFigure2.pdf shows Sea-ice concentration in (A) 6.83-6.85 ka BP and (B) 7.63-7.65 ka BP in the TraCE-21ka. Subsurface (92 m) temperature in (C) 6.81-6.83 ka BP and (D) 7.63-7.65 ka BP in the TraCE-21ka.</p>
Fig. 1 in Osmolality and composition of the extender during the cold storage of Prochilodus lineatus (Characiformes: Prochilodontidae) sperm
Fig. 1. Motility rate (a); curvilinear (VCL; b), straight-line (VSL; c) and average path (VAP; d) velocities of Prochilodus lineatus sperm diluted in two extender compositions (ACP = closed circles; BTS = open circles) and stored at 6-8°C for six days. Undiluted sperm served as control (closed triangle). Each dot and error bar represents mean ± SD; n=15 males. ACP: Powdered Coconut Water™; BTS: Beltsville Thawing Solution™. *Means followed by this symbol, within the same day of analysis, are significantly higher (P<0.05; Tukey).
Fig. 1 in Oxidative stress parameters in juvenile Brazilian flounder Paralichthys orbignyanus (Valenciennes, 1839) (Pleuronectiformes: Paralichthyidae) exposed to cold and heat shocks
Fig. 1. (TBARS), (GST) and (CAT) activity in the liver of Paralichthys orbignyanus juveniles exposed to different temperatures (17.1, 23.0 and 28.8ºC) as a function of time exposition (72 h). Values are expressed as means ± SEM, N=5. aLower case letters indicate significantly different at the different temperatures and same time (P <0.05), determined by two-way ANOVA and by Dunnet test. ACapital letters indicate significantly different at the same temperatures and different times (P <0.05), determined by two-way ANOVA and by Dunnet test.
Plate XXV, Fig. M.1 – River Cold Sense, near Zollhaus (FR), Switzerland, late March. Rare example of type A and type B in near syntopy. Black arrow: nymphal biotope of type A; white arrow: of type B. in Steps towards a revision of the Perla bipunctata Pictet, 1833 species complex (Plecoptera: Perlidae)
Plate XXV, Fig. M.1 – River Cold Sense, near Zollhaus (FR), Switzerland, late March. Rare example of type A and type B in near syntopy. Black arrow: nymphal biotope of type A; white arrow: of type B.
Fig. 3 in Effects of cold-acclimation, pathogen infection, and varying temperatures on insecticide susceptibility, feeding, and detoxifying enzyme levels in Diaphorina citri (Hemiptera: Liviidae)
Fig. 3. Correlations between mean percentage mortality of Diaphorina citri and temperature for field-collected and uninfected D. citri and field-collected and 'Candidatus' Liberibacter asiaticus–infected D. citri, when exposed to chlorpyriphos (A), fenpropathrin (B), imidacloprid (C), thiamethoxam (D), and spinetoram (E).
Fig. 1 in Effects of cold-acclimation, pathogen infection, and varying temperatures on insecticide susceptibility, feeding, and detoxifying enzyme levels in Diaphorina citri (Hemiptera: Liviidae)
Fig. 1. Comparison of cytochrome P450 (A), general esterase (B), and glutathione S-transferase (C) activity levels in laboratory susceptible Diaphorina citri adults at 5 temperatures. For glutathione S-transferase, means with the same uppercase letters are not significantly different from one another for imidacloprid-treated D. citri. Means with the same lowercase letters are not significantly different from one another for spinetoram-treated D. citri.
Fig. 1. A in New record of the cold freshwater dinoflagellate Palatinus apiculatus (Dinophyceae) from the Paldang Reservoir, Korea
Fig. 1. A map of the Paldang Reservoir, Korea. A black circle represents the sampling site. Black arrows represent direction of water flow.
Fig. 3 in New record of the cold freshwater dinoflagellate Palatinus apiculatus (Dinophyceae) from the Paldang Reservoir, Korea
Fig. 3. Scanning electron microscrope micrographs of Palatinus apiculatus isolated from the Paldang Reservoir, Korea. Plates of the theca are indicated, following to Kofoidian plate formula. A: ventral view showing sulcal region; B, C: apical view from the ventral side; D-F: dorsal view showing different wide of suture and variation of the cingular plate (v). Thick black bar in D-F represents each given length. Sa: anterior sulcal plate. Sd: right sulcal plate. Sp: posterior sulcal plate. Ss: left sulcal plate. Scale bar = 10 μm.
Fig. 2 in New record of the cold freshwater dinoflagellate Palatinus apiculatus (Dinophyceae) from the Paldang Reservoir, Korea
Fig. 2. Vegetative cells (A, C) and temporary cysts (B, D) of the Korean Palatinus apiculatus isolated from the Paldang Reservoir. An arrowhead represents an eyespot. Cell size is proportional to a given scale bar (10 μm).
Fig. 4. A maximum likelihood tree constructed from a 28S in New record of the cold freshwater dinoflagellate Palatinus apiculatus (Dinophyceae) from the Paldang Reservoir, Korea
Fig. 4. A maximum likelihood tree constructed from a 28S rDNA dataset of the Korean Palatinus apiculatus and other freshwater dinoflagellates. A total of 5,000 replicates were run for bootstrap analyses. Members of the genus Palatinus are highlighted in orange. The isolate from this study and its GenBank No. are given in bold font.
Fig. 3. A neighbor-joining phylogenetic tree reconstructed from a in Description of unrecorded wild yeasts from soil in Republic of Korea under cold conditions
Fig. 3. A neighbor-joining phylogenetic tree reconstructed from a comparative analysis of 26S rRNA gene sequences showing the relationships of strain PG3-4-10C with closely related species. Bootstrap values (>70%) based on neighbor-joining methods are shown at the branch nodes. Bar, 0.01 substitutions per nucleotide position.
Fig. 2. A neighbor-joining phylogenetic tree reconstructed from a in Description of unrecorded wild yeasts from soil in Republic of Korea under cold conditions
Fig. 2. A neighbor-joining phylogenetic tree reconstructed from a comparative analysis of 26S rRNA gene sequences showing the relationships of strain CY-9-10C with closely related species. Bootstrap values (>70%) based on neighbor-joining methods are shown at the branch nodes. Bar, 0.02 substitutions per nucleotide position.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
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