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Replication Data for: The Associative System of Early-Learned Hebrew Verbs and Body Parts: A Comparative Study with American English
No full textPaper abstract:
This paper compares the associative system of early-learned verbs and body parts in Hebrew with previously published data on American English (Maouene, Josita, Shohei Hidaka & Linda B. Smith. 2008. Body parts and early-learned verbs. Cognitive Science 32(7). 1200–1216). Following the methodology of the former study, 51 Hebrew-speaking college students gave the first body part that came to mind for each of 103 early-learned Hebrew verbs, 81 of which were translational equivalents. Rate of convergence and divergence and underlying patterns were used to make inferences about the constraints at work. Overall convergence (92.3% of the Hebrew data and 93.7% of the English data) reveal similar entropy levels, comparable semantic field shapes of verbs organized by body parts and similar general cluster patterns of verbs by body parts. Most divergence lies in the infrequent responses (offered fewer than 1% of the time) which arise around body parts that are internal, very detailed, very general categorically, used in figurative language, uniquely provided and tend to be subject to cultural taboos. This is a new contribution, as previous work has not quantified the relative proportion of convergent to divergent associations. We discuss how these findings support neural and developmental continuity and stability in the verbal system with respect to the categorization of verbs by body parts cross-culturally.Dataset description:
The dataset consists of two matrices: the first matrix is composed of 101 early-learned American English verbs by 61 body parts as provided by 50 American English speakers. The second matrix displays 103 early-learned Hebrew verbs by 73 body parts provided by 51 Hebrew speakers.
The English data collections was done at Indiana University Bloomington, IN, in 2004. A partial analysis of the data set was published between 2006 and 2008.
The data collection in Hebrew was done at Ono Academic College (in Hebrew: הקריה האקדמית אונו) located in Kiryat Ono, Tel Aviv region, Israel, in 2012. This is the first publication for this data set
Supplements for Devonian–Carboniferous extension and Eurekan inversion along an inherited WNW–ESE-striking fault system in Billefjorden, Svalbard
No full textSupplementary data for Devonian–Carboniferous extension and Eurekan inversion along an inherited WNW–ESE-striking fault system in Billefjorden, Svalbard.Content:
-S1: Description of the late Paleozoic sedimentary successions in central Spitsbergen from the literature.
-S2: (a) Uninterpreted bathymetric data in Billefjorden and (b–d) associated zooms.
-S3: Interpreted seismic sections in Billefjorden showing early Cenozoic duplexes and thrusts (yellow lines), bedding surfaces (dotted white lines) and potential multiples (dashed yellow lines). See Fig. 1 for location. (a) SSW-directed Cenozoic thrust between Phantomodden and Narveneset showing (from south to north) in the southern part a well-developed SSW-verging ramp anticline and an open, symmetric, NNE-tilted detachment/ramp anticline. (b) Top-west to top-west thrust sheet with minor reverse offsets.
-S4: Uninterpreted seismic sections in Billefjorden. See S1 for location.
-S5: Description and interpretation of the upper Paleozoic sedimentary successions on seismic data in Billefjorden.
-Lower Devonian sedimentary rocks of the Siktefjellet and Red Bay and Andrée Land groups
-Uppermost Devonian to Mississippian sedimentary rocks (Billefjorden Group)
-Pennsylvanian to Permian sedimentary rocks (Gipsdalen Group)
-Uppermost Mississippian to Lower Pennsylvanian Hultberget and Ebbadalen formations
-Middle to lowermost Upper Pennsylvanian Minkinfjellet Formation
-Uppermost Middle Pennsylvanian to lowermost Permian Wordiekammen Formation
-Lower Permian Gipshuken Formation
-S6: Depth conversion data including checkshot data from exploration well 7816/12-1 in Reindalspasset (upper left table; Eide et al., 1991), the depth of lithostratigraphic intervals from the well completion report (upper right table), the depth of formations of interest to the present study from the well completion report (middle right table), average velocities of stratigraphic intervals of interest to the present study from Gernigon et al. (2018; lower right table), and calculated stratigraphic thicknesses and depths, and fault offsets in Billefjorden based on velocities from well 7816/12-1 and from Gernigon et al. (2018; lowermost table).
-S7: (a) Uninterpreted and (b) interpreted depth-converted seismic section NP-IS-85-05 through Billefjorden showing the main NNE-dipping shear zone (dashed yellow and grey-shaded), and some of the normal (red) and inverted brittle faults (black), and décollements and detachments (yellow) shown in Figure 4. Notice the gentle dip of the main shear zone. Abbreviation: GaF: Garmaksla fault.
-S8: Bathymetric profiles across NNE–SSW-trending moraine ridges (up) and a fault-related escarpment (down). Notice the contrast between smooth, 2–3 meters high drops in bathymetry across moraine ridges (black arrows) and the abrupt 5 meter drop across the fault-related escarpment (red arrow).
-S9: Bathymetric profiles across Billefjorden showing the N–S-trending ridge (red arrows). Location of the profiles is shown as white lines in supplement S1d. Notice the steep western flank and the smooth and gently east-dipping top and eastern flank of the ridge.
-S10: Satellite images in (A) Narveneset and (B) Brimerpynten (see Figure 1B for locations) showing smooth, high-frequency, gently curving, NNE–SSW- to NNW–SSE-trending lineaments (dotted white lines) most likely representing sub-vertical bedding surfaces within Lower Devonian sedimentary strata (Dallmann et al., 2004a; Dallmann & Piepjohn, 2020) crosscut by discrete, linear to undulating, dominantly WNW–ESE-trending fault-related escarpments (red lines). The legend is common to A and B.
-S11: Field photograph of WNW–ESE-striking brittle faults in Narveneset showing sinistral sense of shear.
-S12: Decreasing tectonic activity from Early Devonian to early Permian times.
-Early Devonian to Mississippian collapse and rift “initiation” phase
-Latest Mississippian to earliest/Early Pennsylvanian “interaction and linkage” phase
-Middle Pennsylvanian “through-going fault zones” phase
-Late Pennsylvanian to earliest Permian latest- to post-rift phase
-Conclusion
-Figure 1 electronic supplement 12
-S13: (A) Calculation of the surface slope angles between Pyramiden and Yggdrasilkampen and Yggdrasilkampen and Asvindalen and of the altitude difference due to the normal dip angle (c. 145 m) and to Eurekan deformation (c. 330 m). (B) Illustration of the calculated surface slope angles (in red) in Billefjorden and of the potential WNW–ESE-trending fold (in fuchsia) along the Adolfbukta fault. Notice the significant altitude drop of the base of the Wordiekammen Formation between the Pyramiden Mountain (c. 850 meters) and northern Yggdrasilkampen (c. 375 meters).
-S14: Outcrop photograph showing south-dipping and southwards thickening Lower Devonian strata of the Wood Bay Formation in Triungen in the hanging wall of the NNE-dipping Hugindalen Fault
Replication Data for: Characterization of Mechanical and Cellular Effects of Rhythmic Vertical Vibrations on Adherent Cell Cultures
No full textFluorescence microscopic (maximum intensity projection) images of the F-actin filaments (stained with Alexa488 phalloidin green-fluorescence dye) of HeLa cell cultures. 63x oil objective was used to review the staining and images were acquired using the SIM mode of the system (ZEISS Elyra PS1). The experimental conditions were No Vibration (NV), Continuous Vibration (CV), Regular Pulse (RP), and Variable Pulse (VP), using a vertical vibration system
Replication Data for: Dataset of motivational factors for using mobile health applications and systems
No full textThis dataset contains responses from a questionnaire about what motivates people to collect and share their health data for research and public health benefits. The online questionnaire was open for data collection between November 2018 and March 2020. The questionnaire was published in a Norwegian, English and French version, and published online. The questionnaire consisted of 38 questions. A total of 814 participants completed the questionnaire
Replication Data for: A panorama of inchoative constructions in Spanish: Cluster analysis as an answer to the near-synonymy puzzle.
No full textThe dataset contains the data for the hierarchical cluster analysis as explained in the article "A panorama of inchoative constructions in Spanish: Cluster analysis as an answer to the near-synonymy puzzle".
The dataset contains the data for the hierarchical cluster analysis as explained in the article "A panorama of inchoative constructions in Spanish: Cluster analysis as an answer to the near-synonymy puzzle". In total, the dataset contains 3955 observations, which are tokens of the inchoative construction for the following auxiliaries: comenzar, empezar, meter, poner, echar(se), liar, arrancar and romper. The data originates from the the Spanish Web corpus (esTenTen18), accessed via Sketch Engine. Only the European Spanish subcorpus was selected. The search syntax that was used to detect the inchoative construction was the following: “[lemma="empezar"] [tag="R.*"]{0,3}"a"[tag="V.*"] within " (replacing the concrete lemma "empezar" by other lemma's for each auxiliary, see Spinc_queries_20221202.txt for all concrete corpus queries). After downloading samples of 10.000 tokens per auxiliary, the samples were manually cleaned. Only 500 tokens per auxiliary were retained in the dataset. Next, the data were annotated for the infinitive observed after the preposition 'a' and for the semantic class to which this infinitive belongs, following the existing ADESSE classification (see below), besides other criteria that are not taken into account for this study. Concretely, the variables 'INF' (infinitive) and 'Class' were used as input for the hierarchical cluster analysis (see data-specific sections below for more information about the variables).</p
Dataset for the article "Magic for the mind’s eye: A promising avenue for more universal design in the art of magic"
No full textDataset and R-scripts for the manuscript "Magic for the mind’s eye: A promising avenue for more universal design in the art of magic" by Ekroll, V., Wünsch, L. & van Lier, R.Summary from the corresponding manuscript:
In the art of conjuring, as well as in cognitive science, potential possibilities for designing magic tricks that are suitable for people who are blind or visually impaired have only rarely been considered. In this article we argue that many magic tricks which are normally presented in a visual way, are not inherently based on visual processes, but instead on systematic illusions and limitations in visual imagery and mental simulations. Accordingly, it should be possible to adapt these tricks for presentation in a non-visual format, which should be suitable for people who are blind or visually impaired. As an initial test of this general approach, we adapted three magic tricks for non-visual presentation and presented them for blindfolded participants. Standard versions of the tricks were also presented to seeing participants. The participants in both groups were asked to indicate how magical they felt the tricks were, as well as whether they had any idea about the secrets behind them. The results suggest that the non-visual versions of the tricks are roughly comparable to the regular visual versions. We conclude that adapting magic tricks based on illusions of imagery for non-visual presentation appears to be a promising avenue for more universal design in the art of magic. We also argue that the illusions of imagery responsible for the experiences of magic evoked presents interesting challenges for basic cognitive science
Survey data for "Mass development of aquatic plants: effects of contrasting management scenarios on a suite of ecosystem services"
No full textThis dataset contains data from extensive questionnaires carried out for the MadMacs project and covers perception of mass development of macrophytes and the willingness to pay for their removal.
The dataset includes responses from questionnaires spanning five sites with different macrophyte species in four countries (Norway, France, Germany and South Africa).
An example of the questionnaire is available in the supplementary material of the corresponding open access article by Thiemer et al. (2023)
Swedish observations of the Aurora Borealis in the period 1716-1732 in contemporaneous scholarly publications
No full textThis dataset gives an overview of all Swedish observations of the aurora borealis that were published in various Latin publications from the first half of the eighteenth century
Replication Data for: Inter-rater reliability of the Silverman and Andersen index
No full textBackground
There are various methods of respiratory support available to optimize respiratory function in preterm infants. Respiratory scoring tools might provide information on which method to choose and the level and duration of support needed. Before implementing a respiratory scoring tool in our clinical practice, we aimed to test the inter- and intra-rater reliability of the Silverman and Andersen index (SA index) among neonatologists and nurses when applied to preterm infants on respiratory support. We also examined the association between the SA index and the electrical activity of the diaphragm (Edi signals)
Replication Data for: When modality and tense meet. The future marker budet ‘will’ in impersonal constructions with the modal adverb možno ‘be possible’
No full textDataset description:
This is a study of examples of Russian impersonal constructions with the modal word možno ‘can, be possible’ with and without the future copula budet ‘will be,’ i.e., možno + budet + INF and možno + INF. The data was collected in 2020-2021 from the old version of the Russian National Corpus (ruscorpora.ru).
In the spreadsheet 01DataMoznoBudet, the data merges the results of four searches conducted to extract examples of sentences with the following construction types: možno + budet + INF.PFV, možno + budet + INF.IPFV, možno + INF.PFV and možno + INF.IPFV. The results for each search were downloaded, pseudorandomized, and the first 200 examples were manually annotated, based on the syntactic analyses given in the corpus. The syntactic and morphological categories used in the corpus are explained here: https://ruscorpora.ru/corpus/main.
In the spreadsheet 01DataZavtraMoznoBudet, the data merges the results of four searches conducted to extract examples of sentences with the following structure: zavtra + možno + budet + INF.PFV, zavtra + možno + budet + INF.IPFV, zavtra + možno + INF.PFV and zavtra + možno + INF.IPFV. All of the examples (103 sentences) were imported to a spreadsheet and annotated manually, based on the syntactic analyses given in the corpus. The syntactic and morphological categories used in the corpus are explained here: https://ruscorpora.ru/corpus/main.Article abstract:
This paper examines Russian impersonal constructions with the modal word možno ‘can, be possible’ with and without the future copula budet ‘will be,’ i.e., možno + budet + INF and možno + INF. My contribution can be summarized as follows. First, corpus-based evidence reveals that možno + INF constructions are vastly more frequent than constructions with copula. Second, the meaning of constructions without the future copula is more flexible: while the possibility is typically located in the present, the situation denoted by the infinitive may be located in the present or the future. Third, I show that the možno + INF construction is more ambiguous and can denote present, gnomic or future situations. Fourth, I identify a number of contextual factors that unambiguously locate the situation in the future. I demonstrate that such factors are more frequently used with the future copula, and thus motivate the choice between the two constructions. Finally, I illustrate the interpretations in a straightforward manner by means of schemas of the type used in cognitive linguistics.</a