dataesr/scientific-paragraphs-categorization huggingface dataset:
lower SES (LSES)) (7 boys and 8 girls of HSES, 8 boys and 6 girls of LSES) of the INPUT project 6 was analysed. The children were video and audio recorded in everyday situations with their main caretakers in their homes in Vienna at four data points at the mean ages 3;1, 3;4, 4;4 and 4;8. The most interactive 30 minutes per recording were transcribed, coded and analysed, which is equivalent to 58 hours of spontaneous speech material. The correct use of Cst (consonant +st) clusters, in a medial and final position was examined, in correlation to the effects of the data point, SES and morpheme boundary. The results demonstrated that the children made significant progress from the third to the fourth data point and also showed a significant effect of the socio-economic status, since LSES children showed lower accuracy.
methoDology To investigate lexical access, four lexical decision tasks were performed. The experiments (LDT 1, 2 and 3) were designed using the behavioural research software E-Prime 3. 0 (Psychology Software Tools, Pittsburgh, PA) and were all carried out on the same Windows laptop  (Freiberger et al. 2015; Korecky-Kröll et al. 2016; Sommer-Lolei et al. 2017). LDT 4 was an online experiment, programmed and provided by URL: https://quest. christiner. at/. Due to the high number of participants that were all tested in one day, we tested on several Windows computers simultaneously. All of the test items were presented to the participants visually, capitalized in the centre of the screen, following a fixation cross. Participants had to decide as accurately and quickly as possible whether the presented string was an existing German word or not.
g. /gr/, /br/), whereas in LDT 2  (Korecky-Kröll et al. 2016 ), LDT 3 (Sommer-Lolei et al. 2017)  and LDT 4, bi-and triconsonantal clusters occurred (e. g. /rtn/, /lst/). The position of the consonant clusters was either in the final (LDT 1) or in a medial position (LDT 2, 3 and 4). For every morphonotactic consonant cluster there existed a phonotactic match (e. g. LDT 2 on compounds: (M+P+) Haus+tier 'domestic animal' vs. (M-P+) Kastanie 'chestnut'). Therefore, we also matched conditions 2 and 4 (e. g. LDT 3 on derivations: (M+P-) Zeig-er 'pointer' vs. (M-P-) Lager 'storage'). Examples of stimuli for each experiment are listed in Table  2 ; for a summarizing overview of the tasks, see Tables  3  and 4. All of the items were balanced for word length, syllables and average word frequency (taken as the number of occurrences from the CELEX, the Austrian Media Corpus (AMC 7  ) and also the Leipzig Deutscher Wortschatz Online databases).
morphonotactic status of consonant clusters (henceforth CC) in the acquisition of L1 French. In order to benefit from the growing number of resources made available by the scientific community, we selected a corpus out of the CHILDES database (MacWhinney 2000), allowing for comparison with L1 acquisition data collected to test the Strong Morphonotactic Hypothesis (SMH) for German  (Freiberger 2007 (Freiberger , 2014)). We then analysed longitudinal data from four children aged 1;6 to 3;0 collected in spontaneous speech interactions between a parent and the target child with a generalized linear mixed model investigating the role of the factors age, position and phonotactic (PH) vs. morphonotactic (MPH) status on the successful pronunciation of the different CCs.
CorpUs seleCtion An increasing number of resources on L1 acquisition have been made available to the scientific community in recent years. For the present study, we referred to the CHILDES database (MacWhinney 2000) and selected a corpus with a comparable recording process to the methodology used by  Freiberger (2014)  in order to test the SMH in L1 German acquisition. The criteria we used were the recording of spontaneous speech interactions between a parent and the target child, an age of onset of 1;6 and regular recordings up to 3;0. The corpus recorded by  Demuth and Tremblay (2008)  (hereafter 'Lyon Corpus') meets these requirements: four children were, on average, recorded bimonthly (Anaïs, Marie, Nathan and Theotime) from an age onset of 1;0 to the age of 3;0 (4;0 for Marie) and the children's utterances have been orthographically and phonetically transcribed in CHAT format  (MacWhinney 2000).
The data summarized in Table  4  show a clear progression of the number of CCs with age for each child. However, bear in mind that these data were obtained with the orthographical tier and remain hypothetical with respect to the actual production of the CCs. As such, they mainly demonstrate the diversification and complexification of the lexicon in each child. Child 1;6-1;8 1;9-1;11 2;0-2;2 2;3-2;5 2;6-2;8 2;9-2;11 3;0-3;2 Qualitative analysis of the words (see Tables I and II in appendix) shows that the first words containing CCs produced by French L1 children are from various categories with an important proportion of nouns (e. g. nounours 'teddy', veste 'jacket', écharpe 'scarf', fleur 'flower', fraise 'strawberry') and interjections/onomatopoeia  (e. g. bravo, oups, vroum, gling, clac, crac)  followed by adverbs or adverbial locutions (e.
proCeDUre Participants were seated 50 cm from the computer screen and asked to perform a 'letter search task'. They were instructed to respond as rapidly and accurately as possible to whether the cluster of letters 'RE' was present or not in the word to be displayed on the screen. Participants responded 'yes' by pressing one of two response buttons with the forefinger of their right hand and 'no' by pressing the other response button with the forefinger of the left hand. The DMDX software  (Forster & Forster 2003)  was used. Each trial consisted of the following sequence of stimuli: the letters to be searched (RE) presented in uppercase (for 700 ms), followed by a fixation mark (1000 ms), a French word in lowercase (50 ms), which, in turn, was replaced by a mask (##########) that remained on the screen until the participant responded (for a maximum of 1500 ms).
ACKNOWLEDGEMENTS This investigation was performed within the  International Cooperation Project  ' Human Behaviour  and  Machine Simulation in the Processing of (Mor)Phonotactics'. We thank the  Austrian Science Fund (FWF) : [I  1394-G23 ] for its support. Sabine Sommer-Lolei  is a recipient of a DOC-team fellowship of the  Austrian Academy of Sciences. Markus Christiner 's investigation is funded within the  Post-DocTrack Programme  of the OeAW. We are sincerely grateful to  Eva Maria Freiberger  who worked as a project collaborator in the first project phase. She designed the LDT 1 and the PDT experiment, collected the data for these experiments and was also involved in their analysis. Furthermore, she did pioneering work on the acquisition of German morphonotactics. We also want to thank  Angelika Wukowits  for supervising and executing one of the experiments together with  Markus Christiner  in the Secondary School for Economic Professions and the  Educational Institution for Elementary Pedagogy at Sancta Christiana in Frohsdorf, Austria , with our special thanks to all students who took part in our task and to the director  Dr.
ACKNOWLEDGEMENTS The present study was made possible through financial support from an  ANR  grant n°  ANR-13-ISH2-0002-02  to  Basilio Calderone  for the  Cooperation Project 'Human Behaviour and Machine Simulation in the Processing of (Mor)Phonotactics'. We would also like to thank  Wolfgang U. Dressler  for helpful comments on an earlier version of the paper and  Sabine Sommer-Lolei  and  Nicola Wood  for careful editing. All remaining errors are ours.
Acknowledgments The author has studied these visitors' inscriptions within the framework of a survey of secondary epigraphy inside the Theban Tombs, carried out under the aegis of the  French Institute for Oriental Archaeology in Cairo  and in collaboration with the  Polish Centre of Mediterranean Archaeology. A full edition and commentary of the documents is forthcoming (Ragazzoli forthcoming a), an extended version of the author's habilitation thesis:  L'Épigraphie  secondaire dans les Tombes thébaines. Ouvrage original présenté pour l'habilitation à diriger des recherches,  Université Paris Sorbonne ,  2016. For preliminary papers see Ragazzoli 2011; 2013;2016; 2017a;2017c; 2018a; 2018b; 2020;Ragazzoli and Frood 2013; Hassan and Ragazzoli forthcoming.
, 2002)  of PyHST2  (Mirone et al. , 2014). Parameters for phase retrieval were intentionally set with low values (δ/β = 50), effectively using the approach as a denoising low-pass filter. From the 32-bit data generated by PyHST2, postprocessing included: data conversion as 16-bit jpeg2000 stack with a compression ratio of 10, using the full 3D histogram and excluding 0. 001% on both extremities; ring correction  (Lyckegaard et al. , 2011). The reconstructed data were imported as jpeg2000 stacks into the software VGStudio Max 3. 4 (Volume Graphics GmbH) installed on a Dell Computer Station Precision T7600 running Windows 7. The 3D-models presented in this work were created from regions of interest using selection tools in VGStudio Max 3. 4. Virtual scan slices and images of the 3Dmodels were rendered in VGStudio Max 3.
ACKNOWLEDGMENTS The authors would like to thank the reviewers for their input, which greatly improved this work. We also thank  Ursula Toom, Tallinn , for help connected with the loan of material. The experiments were performed on beamline ID19 at the  European Synchrotron Radiation Facility (ESRF , proposal ES 581) in Grenoble, France. We acknowledge the  European Synchrotron Radiation Facility  for provision of synchrotron radiation facilities and for assistance in using beamline ID19. T. M. acknowledges the  Department of Geology at TTU  for allowing her to use their facilities for research.
To account for the complexity of real situations, a few studies have assessed the performance of the phosphate treatments in the field  [9, 25, 36, 37]. Various cases of successful application onto real artworks in Italy, Cyprus, Turkey and the Vatican City have been reported  [25] , but only in a few cases detailed scientific data were made available  [9, 36, 37]. In the present paper, we report the results of the first long-term study aimed at systematically evaluating the performance of the phosphate treatment after prolonged exposure in the field. In particular, the objective of the present study was twofold, as illustrated in Fig. 1. First, the field performance of 5 different formulations of the phosphate treatment was evaluated on naturally weathered marble specimens, in comparison with 2 alternative treatments and an untreated reference, for a total of 8 conditions.
The environmental aggressiveness during the 32 months of field exposure (started in May 2017) was evaluated by analyzing environmental data made freely available by Meteo-France. In particular, to estimate the number of freezing-thawing cycles, the daily values of air temperature, relative humidity and rainfall, measured by the closest survey station (located in Orly, about 25 km from the Royal Palace), were analyzed. According to a previously proposed methodology  [34] , freezing was assumed to occur on those days when air temperature dropped below 0 °C and water was present in the stone, because on the same day either rainfall occurred or relative humidity was higher than 80%, so that condensation on the stone surface likely took place. Of course, such assumptions only allow for a rough estimation of the actual freezing of water inside the marble pores and fissures (because environmental data measured close to stone surface would be needed and because the actual freezing temperature inside the stone depends on the pore size  [34] ), but still useful indications on the likelihood of frost-related risk can be derived.
For Guadeloupe, recent macroscopic data on Cedrosan and Barrancoid influenced Saladoid pastes has been provided by a small number of archaeological excavations at Bisdary (Gourbeyre, Basse-Terre) (Hildebrand in  Romon et al. , 2006:  80 but relying on Chancerel in  Etrich et al. , 2003:73-108)  and at Grand Carbet (Capesterre-Belle-Eau, Basse-Terre) (Chancerel in Toledo i  Mur et al. , 2004:32)  for which grog was not attested for. The Guadeloupean test-case, explored in this study, showed the abundance of grog tempered ceramics for the Troumassoid series, and notably the Mamoran sub-series. And even if we underline that future microscopical analysis is needed for both Saladoid and Troumassoid sites on various islands in order to pin-point the inception data and place of arrival of grog tempered ceramics in the Lesser Antillean arch, we can confirm already part of the  Donahue et al.
Acknowledgements. The authors would like to thank the Inrap excavation teams for the fieldwork done at the three sites. We intend to continue this quest by sampling sherds taken from secure dated features from different sites in the French West Indies (Martinique, Marie-Galante, Guadeloupe, Saint-Barth and Saint-Martin). The authors wish to thank the two anonymous reviewers for their comments on the article and to John G. Crock for the English improvements. The authors have no conflict of interest to declare. Furthermore, we would also like to invite researchers working on the other islands to join us.
Acknowledgements: This article is the translated and slightly modified version of the article published originally as:  Philippe Corcuff , " Les séries TV comme nouvelles théories critiques en contexte identitariste et ultraconservateur. American Crime ,  The Sinner ,  Sharp Objects ,  Unorthodox. "TV/Series 19 (2021), DOI: https://doi. org/10. 4000/tvseries. 5133;URL: http://journals. openedition. org/tvseries/5133. The text was translated by  Daniela Ginsburg  and edited by  Jennie Rothwell.
In this publication, we present a non-intrusive, multidisciplinary approach using mainly marine geophysical data implemented at the coastal zone of Aegina city in the framework of the "Aigina Harbour-city Project". Multibeam, side-scan sonar, and subbottom profiler acoustic data were used to map and delimit the ancient coastal installations and study the geomorphology of the area in detail. Detection of the submerged ancient harbour facilities (conical rubble structures and breakwaters) spatial extent and distribution analysis was performed using the acoustic data in combination with automatic seafloor segmentation techniques, allowing the preliminary interpretation hypotheses regarding their use in antiquity (defensive/sheltering function) but also of sea-level change scenarios. Parametrization of the submerged archaeological remains contributed to their morphometric analysis (geometric characteristics and depth distribution of the structures, burial depth, construction morphologies), but also helped in assessing their preservation status since the modern harbour activities affect them directly, setting several of them under great risk.
Methodology The methodology followed in this marine geological prospection started from an overall approach to the area of interest using marine remote sensing techniques for mapping the acoustic/geomorphological properties of the seafloor and the stratigraphy. Automatic segmentation techniques were implemented for the detection of sites of possible archaeological interest and were validated through acoustic data thereafter. Ground truthing of those areas was finally performed using a Remotely Operated Vehicle (ROV) which was also used for implementing photogrammetric techniques on one of the findings. The methodological approach followed in this article has been extensively described by N. Georgiou in the following article  [35].
The swath width of the SSS was set at 100 m, while the lane spacing was 25 m, providing a 75% range overlap. Data were mosaiced using the SeaView Mosaic (Moga software). The thickness of the sedimentary unit and the seismic stratigraphy was obtained through the "Chirp" Kongsberg Geoacoustics Geopulse Plus sub-bottom profiler system with a Universal transceiver, an acquisition display, and an over-the-side Transducer Mounting (array of 4 transducers) with a hydrophone. The operating frequencies ranged between 1. 5-11. 5 kHz using the hyperbolic chirp pulses, which achieve greater penetration with a maximum vertical resolution of 10 cm. The positioning of the vessel and data georeference were accomplished through a Leica GS08 RTK GNSS that provided an accuracy of 10 mm. The HYPACK software was used for the navigation of the vessel.
Detection and Parametrization of Submerged Antiquities For the detection of possible archaeological targets, the bathymetric slope was converted to a greyscale image with a pixel size of 1. 2 m, to be further processed in the TargAn software  [36, 37]  for segmentation and statistical parameterization (Section 4. 2. 1). The "Canny" edge detection method, as adopted in the TargAn software was the core of the segmentation process. The "Canny" method (1986) finds edges by looking for local maxima of the gradient of the processed image. The gradient is calculated using the derivative of a Gaussian filter. The method uses two thresholds, to detect strong and weak edges, and includes the weak edges in the output only if they are connected to strong edges while it is relatively insensitive to noise.
Photogrammetric Implications Ground-truthing of the areas of interest was attained using a SubseaTech mini ROV Guardian. The exact position of the ROV was achieved by utilizing a Blueprint subsea X150 USBL acoustic transponder attached to it. A carbon fiber tube was also added at the front part of the ROV where 3 action cameras (GoPro 7) were embedded. The 2 side cameras were placed at a 30 • angle on the Y-axis and 45 • on the X-axis so that they both focus on the front and center view. The middle camera was also inclined 30 • on the Y-axis while it remained centered on the front. The cameras were synchronized and set to record high-quality video (1920 × 1080 px). By acquiring footage from 3 different cameras and 3 different angles a very dense set of overlapping images was collected. The post-processing of the data collected was performed using Agisoft Metashape ® software (v.
oceanica field is present in the southern area, mostly at the very shallow eastern part, while moving to the east it is present only around the breakwater and the two mounds. The thickness of the sedimentary unit close to the breakwater varies from 0. 5-1. 5 m while at the area of the two mounds the maximum thickness (>4. 5 m) appears (Figure  5E ). South of the breakwater the rocky bedrock outcrops at a depth of 1. 9 m and inclines at an average angle of 4 •. The rest of the seafloor is mostly sandy while it inclines gently (1 • ) towards the west. For the automatic detection of the submerged ancient port structures; as described in the methodological part, the bathymetric slope was converted to a greyscale image and was processed in the TargAn software  [36, 37]  for segmentation and statistical parameterization (Figure  6 ).
The software segmented multiple areas along the Aegina coastline which matched the areas of the submerged harbour facilities. The north and south breakwaters were detected successfully as well as the conical rubble structures. The two mounds also described in Section 4. 1. 3 were also detected by TargAn and were grouped with the rest of the targets. However, in one of the segmented areas, the software detected features irrelevant to the archaeological targets. This area was outside the modern harbour facilities where dredging has exposed the bedrock, creating strong edges that were included in the segmented areas. To add to that, the limitation of the analyzed slope image resolution which was 1. 2 m, did not allow the detection of targets of possible archaeological interest, with a dimension lower than the image resolution.
To avoid these effects and reach a final delimitation of the ancient structures, all of the geophysical and visual data were interpreted and combined with the results of the segmentation process. The map that contains the final delimitation of the ancient harbour facilities is given in Section 4. 2. 2. For the automatic detection of the submerged ancient port structures; as described in the methodological part, the bathymetric slope was converted to a greyscale image and was processed in the TargAn software  [36, 37]  for segmentation and statistical parameterization (Figure  6 ). The software segmented multiple areas along the Aegina coastline which matched the areas of the submerged harbour facilities. The north and south breakwaters were detected successfully as well as the conical rubble structures.
The two mounds also described in Section 4. 1. 3 were also detected by TargAn and were grouped with the rest of the targets. However, in one of the segmented areas, the software detected features irrelevant to the archaeological targets. This area was outside the modern harbour facilities where dredging has exposed the bedrock, creating strong edges that were included in the segmented areas. To add to that, the limitation of the analyzed slope image resolution which was 1. 2 m, did not allow the detection of targets of possible archaeological interest, with a dimension lower than the image resolution. To avoid these effects and reach a final delimitation of the ancient structures, all of the geophysical and visual data were interpreted and combined with the results of the segmentation process.
3 m of loose sediment. 67% of the cones' crests were found at a depth range of 3. 6-4. 1 m while the rest ranged from 2. 9-5 m. The height (h) of most of the cones varied from 5. 7-7. 5 m while at the southern part they presented a minimum height of 3. 6-4. 1 m. It was observed that the greater the depth of the acoustic bedrock, the greater was the height of each conical structure. As already mentioned in Section 4. 2. 1 the conical structures were constructed in two construction morphologies, the single and the multiple whose morphometric properties were realized through the TargAn software. It was calculated that the single cones were slightly bigger than the multiple morphology conical structures. Single cones presented an upper radius (r) range of 11. 5-12. 5 m while their base radius (R) ranged between 12.
Condition Assessment of the Submerged Archaeological Remains The modern harbour of Aegina is the receiver of a great number of vessels and especially passenger vessels whose density was estimated at an average of more than 1000 h/km 2 (EMODNET-vessel density map, accessed on 26 May 2021). The passenger vessels have an average draught of 3. 5-4 m, while they affect the seafloor with water turbulence and mechanical disturbance. The shape geometry and terrain statistical parameters of the segmented objects (i. e. , conical rubble structures and breakwaters) as derived by the TargAn software, were data mined against their ability to reveal any meaningful spatial patterns related to their preservation status or their geometrical distribution. Although no spatial pattern was revealed using any of the shape geometry statistics, the standard deviation and depth range within the interior plus a buffer of 5 m around each segmented object showed a clear spatial pattern.
Relative Sea-Level Rise Implications The survey provided more accurate data for advancing the issue of the relative sealevel change in Aegina that remains open. Submerged archaeological remains in the Attico-Cycladic massive, including the Sounion area, (-2. 5 to -3 m bpsl during the Classical and Hellenistic period  [17, 59, 60] ), suggest that a sea-level rise rate of 1-1. 2 mm/yr affected the area during the last 2. 5 ka  [17, 59, 60]. Different relative sea-level scenarios have been advanced for the city of Aegina  [3, 4]. When using the data of the current survey and assuming that the depth of the well-preserved conical rubble structures' crests remained intact through the centuries, all the well-preserved crests' depth range between 3. 2-4. 4 m bpsl with a mean value of -3. 9 m bpsl.