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FIGURE 3 in Description and ontogeny of Pattersoncypris minima sp. nov. (Crustacea Ostracoda), Araripe Basin, Northeast Brazil

FIGURE 3. Length versus height plots for Pattersoncypris minima sp. nov. showing its different growth stages. A structural histogram of the assemblage was made to analyze the abundance of each instar (Fig. 2). Height and

opennotspecifiedSep 2020View details →
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FIGURE 2 in Description and ontogeny of Pattersoncypris minima sp. nov. (Crustacea Ostracoda), Araripe Basin, Northeast Brazil

FIGURE 2. Population histogram according to ontogenetic stages present in the studied assemblage of Pattersoncypris minima sp. nov.

opennotspecifiedSep 2020View details →
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FIGURE 1 in Description and ontogeny of Pattersoncypris minima sp. nov. (Crustacea Ostracoda), Araripe Basin, Northeast Brazil

FIGURE 1. Map of the study area showing the collection location in the Araripe Basin, NE of Brazil. (Produced from metadata provided by Geological Survey of Brazil-CPRM).

opennotspecifiedSep 2020View details →
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FIGURE 3 in New species and stages description of Traverella Edmunds, 1948 (Ephemeroptera Leptophlebiidae) from Northeast Brazil

FIGURE 3. Traverella excelsior sp. nov. nymph; A) habitus; B) detail of abdominal sterna; C) lateral view of nymph. Scale bars in mm: A–C = 2.

opennotspecifiedOct 2020View details →
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FIGURE 2 in New species and stages description of Traverella Edmunds, 1948 (Ephemeroptera Leptophlebiidae) from Northeast Brazil

FIGURE 2. Traverella excelsior sp. nov. male imago; (A–B) Wings: A) forewing; B) hind wing; C) enlarged hind wing; (D–E) Genitalia: D) ventral view; E) detail of penes, ventral view. Scale bars in mm: A = 2; B = 0,5; D–E = 0,2.

opennotspecifiedOct 2020View details →
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FIGURE 6 in New species and stages description of Traverella Edmunds, 1948 (Ephemeroptera Leptophlebiidae) from Northeast Brazil

FIGURE 6. Traverella maranhensis. nymph; A) habitus; B) lateral view of head (arrow indicating the clypeal projection); C) detail of abdominal sterna; D) lateral view of nymph. Scale bars in mm: A, C and D = 2; B = 0,5.

opennotspecifiedOct 2020View details →
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FIGURE 8 in New species and stages description of Traverella Edmunds, 1948 (Ephemeroptera Leptophlebiidae) from Northeast Brazil

FIGURE 8. Traverella maranhensis. nymph; A) foreleg; B) anterior tarsal claw; C) middle leg; D) Gill IV; E) hind leg. Scale bars in mm: A, C and E = 1; B = 0,2; D = 0,5.

opennotspecifiedOct 2020View details →
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FIGURE 7 in New species and stages description of Traverella Edmunds, 1948 (Ephemeroptera Leptophlebiidae) from Northeast Brazil

FIGURE 7. Traverella maranhensis. nymph; A) labrum, dorsal view; B) hypopharynx, ventral view; C) labium, dorsal view; D) left mandible; E) maxilla, ventral view. Scale bars in mm: A–E = 0,5.

opennotspecifiedOct 2020View details →
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FIGURE 4 in New species and stages description of Traverella Edmunds, 1948 (Ephemeroptera Leptophlebiidae) from Northeast Brazil

FIGURE 4. Traverella excelsior sp. nov. nymph; A) labrum, dorsal view; B) hypopharynx, ventral view; C) labium, dorsal view; D) left mandible; E) maxilla, ventral view. Scale bars in mm: A–E = 0,5.

opennotspecifiedOct 2020View details →
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FIGURE 5 in New species and stages description of Traverella Edmunds, 1948 (Ephemeroptera Leptophlebiidae) from Northeast Brazil

FIGURE 5. Traverella excelsior sp. nov. nymph; A) foreleg; B) middle leg; C) Gill IV; D) hind leg; E) hind tarsal claw. Scale bars in mm: A, B and D = 1; C = 0,5; E = 0,2.

opennotspecifiedOct 2020View details →
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FIGURE 1 in New species and stages description of Traverella Edmunds, 1948 (Ephemeroptera Leptophlebiidae) from Northeast Brazil

FIGURE 1. Traverella excelsior sp. nov. male imago; A) lateral view of imago; B) head (dorsal view); C) thorax and abdomen (dorsal view); D) genitalia (ventral view); E) abdominal segments VII–X (lateral view). Scale bars in mm: A = 2; B, E = 0,5; C = 1; D = 0,2.

opennotspecifiedOct 2020View details →
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FIGURES 1–4 in A new species of Miccolamia Bates, 1884 (Coleoptera: Cerambycidae: Lamiinae) from northeast India, with comments on related species

FIGURES 1–4. Miccolamia arunachalensis sp. nov. 1, Dorsal habitus; 2, Ventral habitus; 3, Lateral habitus; 4, Details of anterior half in dorso-lateral view; note hump-like pronotum and prominent subbasal elytral tubercles.

opennotspecifiedOct 2020View details →
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Out-of-phase Decadal Change in Drought over Northeast China between Early Spring and Late Summer around 2000 and Its Linkage to the Atlantic Sea Surface Temperature

<p>This file is for the upload of CN05.1 data for&nbsp;2020JD034048R.</p>

opencc-by-4.0Jan 2021View details →
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FIGURE 3 in Description and ontogeny of Pattersoncypris minima sp. nov. (Crustacea Ostracoda), Araripe Basin, Northeast Brazil

FIGURE 3. Length versus height plots for Pattersoncypris minima sp. nov. showing its different growth stages

opennotspecifiedSep 2020View details →
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Data from: Seasonal dynamics of spatial distribution and overlap between Northeast Arctic cod (Gadus morhua) and capelin (Mallotus villosus) in the Barents Sea

The trophic link between cod (Gadus sp.) and capelin (Mallotus sp.) is important in many panarctic ecosystems. Since the early 2000s, the Northeast Arctic cod stock (G. morhua) in the Barents Sea has increased greatly, and the sea has been exceptionally warm. Such changes have potentially large effects on species distributions and overlap, which in turn could affect the strength of species interactions. Due to its high latitude location, the Barents Sea has strong seasonal variation in physical conditions and interactions. To study drivers of variation in cod-capelin overlap, we use data from two annual surveys run in winter and in autumn of 2004-2015. We first model winter and autumn spatial distributions of mature and immature cod and capelin. We then calculate overlap from model predictions on a grid with similar spatial resolution as the survey data. Our approach allowed us to interpret changes in overlap as species-specific effects of stock size and temperature, while accounting for sampling variation due to sampling time and depth. We found that during winter both species expanded their distribution in response to increased stock sizes, but how strongly and where the expansion occurred varied. The effect of temperature on distributions varied in space, and differed for cod and capelin and for different components of the two species. The results for autumn were clearer and more consistent. Both species expanded their distribution areas as their stock sizes increased. A positive effect of temperature was found in the north-eastern Barents Sea, where temperatures were lowest at the start of the study. Overlap increased and shifted north-eastwards during the study period and remained high despite a decline in the capelin stock. The increased overlap during autumn could mainly be attributed to the shift in cod distribution with increased cod stock biomass.

opencc-zeroDec 2017View details →
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Data from: Disassembly of an epibenthic assemblage in a sustained severely hypoxic event in a northeast Pacific basin

As global ocean deoxygenation proceeds and the frequency of extreme low-oxygen (hypoxic) events increases, seafloor ecosystems will inevitably be affected. Our study examines how benthic community responses scale with the severity and spatial extent of hypoxia. Saanich Inlet is a natural model system for testing the effects of hypoxic conditions that determine the benthic megafaunal community structure during annual deoxygenation and reoxygenation. In 2016, an anomalously severe and widespread hypoxic event occurred in the fjord after a decade of oxygen decline at a rate of 0.07 mL L−1 y−1 as measured by a cabled seafloor observatory. We use a living ecological time-series generated from remotely operated vehicle surveys to assess how the benthic megafaunal community disassembled in response to this extreme hypoxic event. Three benthic surveys at similar times in 2013 and 2016 reveal large increases in the area of seafloor bathed in anoxic and hypoxic waters in the latter year. Both bottom oxygen and species depth distributions shoaled from 2013 to 2016, accompanied by a 56% overall decline in megafauna. The abundant habitat-forming pennatulacean octocoral, Halipteris willemoesi, decreased in abundance by 92.3% from fall 2013 to fall 2016, and pandalid shrimp disappeared from the community. Hypoxia-tolerant species experienced milder losses, and two new species occurred in 2016 – one a predator on the coral. Co-occurrence analyses revealed loss of significant community segregation from 2013 to 2016, and a re-mix of pairwise species co-occurrences in the latter year. The loss of oxygenated habitat compressed species into narrower depth ranges and led to disassembly probably through niche space constriction, while decimation of some populations eliminated key community associations. Community fragmentation and disruption of interactions is a possible outcome for many marine benthic ecosystems as marine hypoxia intensifies.

opencc-zeroJun 2019View details →
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Data from: SNPs reveal a genetic cline across the northeast Atlantic and enable powerful population assignment in the European lobster

Resolving stock structure is crucial for fisheries conservation to ensure that the spatial implementation of management is commensurate with that of biological population units. To address this in the economically important European lobster (Homarus gammarus), genetic structure was explored across the species' range using a small panel of single nucleotide polymorphisms (SNPs) previously isolated from restriction-site associated DNA sequencing; these SNPs were selected to maximise differentiation at a range of both broad- and fine-scales. After quality control and filtering, 1,278 lobsters from 38 sampling sites were genotyped at 79 SNPs. The results revealed a pronounced phylogeographic break between the Atlantic and Mediterranean basins, while structure within the Mediterranean was also apparent, partitioned between lobsters from the central Mediterranean and the Aegean Sea. In addition, a genetic cline across the northeast Atlantic was revealed using both putatively neutral and outlier SNPs, but the precise driver(s) of this clinal pattern –isolation-by-distance, secondary contact, selection across an environmental gradient, or a combination of these factors– remains undetermined. Putatively neutral markers differentiated lobsters from Oosterschelde, an estuary on the Dutch coast, a finding likely explained by past bottlenecks and limited gene flow with adjacent North Sea populations. Building on the findings of our spatial genetic analysis, we were able to test the accuracy of assigning lobsters at various spatial scales, including to basin of origin (Atlantic or Mediterranean), region of origin and sampling location. The predictive model assembled using 79 SNPs correctly assigned 99.7 % of lobsters not used to build the model to their basin of origin, but accuracy decreased to region of origin and again to sampling location. These results are of direct relevance to managers of lobster fisheries and hatcheries, and provide the basis for a genetic tool for tracing the origin of European lobsters in the food supply chain.

opencc-zeroJul 2019View details →
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Data from: Bioenergetics modeling of the annual consumption of zooplankton by pelagic fish feeding in the Northeast Atlantic

The present study uses bioenergetics modeling to estimate the annual consumption of the main zooplankton groups by some of the most commercially important planktivorous fish stocks in the Northeast Atlantic, namely Norwegian spring-spawning (NSS) herring (Clupea harengus), blue whiting (Micromesistius poutassou) and NEA mackerel (Scomber scombrus). The data was obtained from scientific surveys in the main feeding area (Norwegian Sea) in the period 2005-2010. By incorporating novel information about ambient temperature, seasonal growth and changes in the diet from stomach content analyses, annual consumption of the different zooplankton groups by pelagic fish is estimated. The present study estimates higher consumption estimates than previous studies for the three species and suggests that fish might have a greater impact on the zooplankton community as foragers. This way, NEA mackerel, showing the highest daily consumption rates, and NSS herring, annually consume around 10 times their total biomass, whereas blue whiting consume about 6 times their biomass in zooplankton. The three species were estimated to consume an average of 135 million (M) tonnes of zooplankton each year, consisting of 53-85 M tonnes of copepods, 20-32 M tonnes of krill, 8-42 M tonnes of appendicularians and 0.2-1.2 M tonnes of fish, depending on the year. For NSS herring and NEA mackerel the main prey groups are calanoids and appendicularians, showing a peak in consumption during June and June-July, respectively, and suggesting high potential for inter-specific feeding competition between these species. In contrast, blue whiting maintain a low consumption rate from April to September, consuming mainly larger euphausiids. Our results suggest that the three species can coexist regardless of their high abundance, zooplankton consumption rates and overlapping diet. Accordingly, the species might have niche segregation, as they are species specific, showing annual and inter-annual variability in total consumption of the different prey species. These estimates and their inter-annual and inter-specific variation are fundamental for understanding fundamental pelagic predator-prey interactions as well as to inform advanced multispecies ecosystem models.

opencc-zeroDec 2017View details →
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Data from: Accuracy of assignment of Atlantic salmon (Salmo salar L.) to rivers and regions in Scotland and northeast England based on single nucleotide polymorphism (SNP) markers.

Understanding the habitat use patterns of migratory fish, such as Atlantic salmon (Salmo salar L.), and the natural and anthropogenic impacts on them, is aided by the ability to identify individuals to their stock of origin. Presented here are the results of an analysis of informative single nucleotide polymorphic (SNP) markers for detecting genetic structuring in Atlantic salmon in Scotland and NE England and their ability to allow accurate genetic stock identification. 3,787 fish from 147 sites covering 27 rivers were screened at 5,568 SNP markers. In order to identify a cost-effective subset of SNPs, they were ranked according to their ability to differentiate between fish from different rivers. A panel of 288 SNPs was used to examine both individual assignments and mixed stock fisheries and eighteen assignment units were defined. The results improved greatly on previously available methods and, for the first time, fish caught in the marine environment can be confidently assigned to geographically coherent units within Scotland and NE England, including individual rivers. As such, this SNP panel has the potential to aid understanding of the various influences acting upon Atlantic salmon on their marine migrations, be they natural environmental variations and/or anthropogenic impacts, such as mixed stock fisheries and interactions with marine power generation installations.

opencc-zeroDec 2015View details →
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Data from: The dynamics of Kelp Forests in the Northeast Pacific Ocean and the relationship with environmental drivers

1.The dynamics of foundation species in ecosystems are key to the fate of many species. Kelp forests are foundation species in temperate ocean ecosystems and contribute to carbon storage, macronutrient dynamics, primary production, and biodiversity of myriad associated species. Downward trends in their abundance globally have been of concern. 2.We analyzed 26 years of aerial censuses (1989-2015) of 2 canopy kelp species in Washington State (USA) waters. We compared these modern censuses with censuses in 1911 and 1912 to determine the persistence of kelp cover over the past century. Using Auto-regressive Integrated Moving Average (ARIMA) models, we compared kelp dynamics with likely environmental drivers, including local environmental variables and ocean indices for this region. 3.Kelp remains at historic levels in many areas, though some eastern populations in proximity to greater human populations are the exception to this pattern. Over the last 26 years, kelp abundance showed high spatial autocorrelation in western areas of Straits of Juan de Fuca, with more variable populations in the annual species and eastward toward Puget Sound. Both species covaried positively in their abundance throughout most of the study area, suggesting environmental factors rather than competition, drove their dynamics. The population dynamics of these kelp species showed that the abundance one year previous was an important predictor, and cyclic dynamics were not indicated using Auto-regressive Integrated Moving Average (ARIMA) models. Kelp abundance correlated inversely with the Pacific Decadal Oscillation and the Oceanic Nino Index, and positively with the North Pacific Gyre Oscillation, indicating that large-scale processes associated with colder seawater temperatures were associated with greater relative abundance of kelp. 4.Synthesis. Kelp beds in the northern California Current Large Marine Ecosystem have mostly remained persistent over the past century and over many km, but some areas may have decreased in abundance. The sensitivity of these populations to indices of ocean climate, our demonstration that a historic 93-year SST record (Race Rocks, Canada) showed a 0.72°C increase, and the classification of some areas as high variability-low abundance, suggest that the viability of these foundational species remain a concern into the future.

opencc-zeroDec 2016View details →

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Last verified 2026-04-30Open record

International Brain Laboratory public data

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Last verified 2026-04-29Open record

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neuroscienceopenPublished datasets are available on demand over the internet.
Last verified 2026-04-29Open record

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