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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Chersoni, Emmanuele; Santus, Enrico; Lenci, Alessandro; Blache, Philippe; +1 Authors

    Several studies on sentence processing suggest that the mental lexicon keeps track of the mutual expectations between words. Current DSMs, however, represent context words as separate features, thereby loosing important information for word expectations, such as word interrelations. In this paper, we present a DSM that addresses this issue by defining verb contexts as joint syntactic dependencies. We test our representation in a verb similarity task on two datasets, showing that joint contexts achieve performances comparable to single dependencies or even better. Moreover, they are able to overcome the data sparsity problem of joint feature spaces, in spite of the limited size of our training corpus. Comment: 5 pages

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ arXiv.org e-Print Ar...arrow_drop_down
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    arXiv.org e-Print Archive
    Other literature type . Preprint . 2016
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    https://doi.org/10.18653/v1/d1...
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ arXiv.org e-Print Ar...arrow_drop_down
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      arXiv.org e-Print Archive
      Other literature type . Preprint . 2016
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: R. Ma; R. Ma; S. Sépulcre; L. Licari; +4 Authors

    Abstract. We have measured Cd/Ca ratios of several benthic foraminiferal species and studied benthic foraminiferal assemblages on two cores from the northern Indian Ocean (Arabian Sea and northern Bay of Bengal, BoB), in order to reconstruct variations in intermediate-water circulation and paleo-nutrient content since the last deglaciation. Intermediate water Cdw records estimated from the benthic Cd/Ca reflect past changes in surface productivity and/or intermediate–bottom-water ventilation. The benthic foraminiferal assemblages are consistent with the geochemical data. These results suggest that during the last deglaciation, Cdw variability was primarily driven by changes in intermediate-water properties, indicating an enhanced ventilation of intermediate–bottom water masses during both Heinrich Stadial 1 and the Younger Dryas (HS1 and YD, respectively). During the Holocene, however, surface primary productivity appears to have influenced Cdw more than intermediate water mass properties. This is evident during the early Holocene (from 10 to 6 cal ka) when benthic foraminiferal assemblages indicate that surface primary productivity was low, resulting in low intermediate-water Cdw at both sites. Then, from ∼ 5.2 to 2.4 cal ka, surface productivity increased markedly, causing a significant increase in the intermediate-water Cdw in the southeastern Arabian Sea and the northeastern BoB. The comparison of intermediate-water Cdw records with previous reconstructions of past Indian monsoon evolution during the Holocene suggests a direct control of intermediate-water Cdw by monsoon-induced changes in upper-water stratification and surface primary productivity. International audience

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ ArchiMer - Instituti...arrow_drop_down
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    https://cp.copernicus.org/prep...
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    Climate of the Past (CP)
    Article . 2022 . Peer-reviewed
    License: CC BY
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    https://doi.org/10.5194/cp-202...
    Preprint . 2020 . Peer-reviewed
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    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Climate of the Past (CP)
    Other literature type . 2021
    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Climate of the Past
    Article . 2022
    Data sources: DOAJ
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ ArchiMer - Instituti...arrow_drop_down
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      https://cp.copernicus.org/prep...
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      Climate of the Past (CP)
      Article . 2022 . Peer-reviewed
      License: CC BY
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      https://doi.org/10.5194/cp-202...
      Preprint . 2020 . Peer-reviewed
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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      Climate of the Past (CP)
      Other literature type . 2021
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
      Climate of the Past
      Article . 2022
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Pedro Cermeño; Carmen García-Comas; Alexandre Pohl; Simon Williams; +6 Authors

    21 pages, 3 figures, supplementary information https://doi.org/10.1038/s41586-022-04932-6.-- Data availability: Fossil diversity digitized data and those data downloaded from the Sepkoski’s Online Genus Database (http://strata.geology.wisc.edu/jack/) are provided as source data with this paper. Diversity data downloaded from the Ocean Biodiversity Information System (OBIS) database (www.obis.org) are also provided as source data with this paper. Source data are provided with this paper.-- Code availability: The coupled palaeogeographical–diversification model presented here uses input data of seafloor age distributions and palaeoenvironmental conditions from the siwill22/agegrid-0.1 v1-alpha palaeogeographical model and the cGENIE Earth system model, respectively. The code used to reconstruct seafloor age distributions from GPlates full-plate tectonic reconstructions is available at Zenodo (https://doi.org/10.5281/zenodo.3271360). The code for the version of the ‘muffin’ release of the cGENIE Earth system model used in this paper is tagged as v0.9.30, and is available at Zenodo (https://doi.org/10.5281/zenodo.6676435). Configuration files for the specific experiments presented in the paper can be found in the directory: genie-userconfigs/PUBS/published/Cermeno_et_al.2022. Details of the experiments, plus the command line needed to run each one, are given in the readme.txt file in that directory. The code for the muffingen boundary file generator, is available at Zenodo (https://doi.org/10.5281/zenodo.6676451). The code for the coupled palaeogeographical–diversification model is available at Zenodo (https://doi.org/10.5281/zenodo.6535496). The code is also available at GitHub (https://github.com/CarmenGarciaComas/INDITEK); this is the recommended mode of access as it will contain any updates and clarifications The fossil record of marine invertebrates has long fuelled the debate as to whether or not there are limits to global diversity in the sea1,2,3,4,5. Ecological theory states that, as diversity grows and ecological niches are filled, the strengthening of biological interactions imposes limits on diversity6,7. However, the extent to which biological interactions have constrained the growth of diversity over evolutionary time remains an open question1,2,3,4,5,8,9,10,11. Here we present a regional diversification model that reproduces the main Phanerozoic eon trends in the global diversity of marine invertebrates after imposing mass extinctions. We find that the dynamics of global diversity are best described by a diversification model that operates widely within the exponential growth regime of a logistic function. A spatially resolved analysis of the ratio of diversity to carrying capacity reveals that less than 2% of the global flooded continental area throughout the Phanerozoic exhibits diversity levels approaching ecological saturation. We attribute the overall increase in global diversity during the Late Mesozoic and Cenozoic eras to the development of diversity hotspots under prolonged conditions of Earth system stability and maximum continental fragmentation. We call this the ‘diversity hotspots hypothesis’, which we propose as a non-mutually exclusive alternative to the hypothesis that the Mesozoic marine revolution led this macroevolutionary trend12,13 This work was funded by research grant CGL2017-91489-EXP from the Spanish government. A.P. acknowledges funding from the European Union’s Horizon research and innovation programme under the Marie Skłodowska-Curie grant agreement no. 838373. S.W. was supported by NSFC grant no. 41972237 and ARC grant nos DP180102280 and DP200100966. M.J.B. acknowledges support through ERC Advanced Grant ‘Innovation’ (ERC 788203). P.C. and S.M.V. acknowledge support through grant no. CTM2017-87227-P. A.R. acknowledges NSF grant EAR-2121165, as well as support from the Heising–Simons Foundation. The Institut de Ciències del Mar (CSIC) received funding from the Spanish government through the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S) Peer reviewed

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ HAL AMU; Mémoires en...arrow_drop_down
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    Nature
    Other literature type . Article . 2022 . Peer-reviewed
    License: CC BY
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    Nature
    Article . 2021
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ HAL AMU; Mémoires en...arrow_drop_down
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      Nature
      Other literature type . Article . 2022 . Peer-reviewed
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      Nature
      Article . 2021
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Trépied, Benoît; Muckle, Adrian;

    ABSTRACT For more than a century, from the 1870s to the 1980s, stockmen were important intermediaries and figures of power and influence in the construction, maintenance and renewal of the colonial order in New Caledonia. Social relations between Kanak and settlers working in the cattle ‘runs’ permitted a unique form of mobility spanning the frontier. The relations developed between chiefs and cattle farmers are central to the processes by which certain administrative chieftaincies emerged in the late‐nineteenth century, and by which Kanak entered the ‘political’ sphere in the second half of the twentieth century. With reference to the locality of Koné, this article traces the political alliances fashioned between Kanak stockmen and their employers in the context of colonisation, rebellion, evangelisation, post‐war political emancipation, local development and, finally, the struggle between supporters and opponents of independence in the 1980s.

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    Oceania
    Article . 2010 . Peer-reviewed
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    Authors: Thibaud Saos; Sophie Grégoire; Jean-Jacques Bahain; Thomas Higham; +11 Authors

    This paper presents new archaeological material and first dates on Upper Pleistocene layers at the site of La Crouzade cave (Gruissan, Aude, France). The site was first excavated by T. and P. Héléna at the beginning of the twentieth century, and the excavations were recently completed during three years (2016–2018) of systematic campaigns. We obtained dates from Middle Palaeolithic layers using two methods: AMS 14C dates were obtained from bone and charcoal, and combined ESR-U series dating was undertaken on horse teeth. Together, these methods allowed us to date this Mousterian sequence to 49,776–44805 cal BP for the deepest level (layer C8) and from 42,000 ± 3000 years BP for the top (layer C6). The Upper Palaeolithic layers are preserved only as patches in the actual excavation area, but a date was obtained from a piece of charcoal collected from a small hearth preserved in the first layer (C5) above Middle Palaeolithic deposits, which indicates an age similar to that of a modern human maxillary previously analysed and re-dated here from 36,014 to 34402 cal BP, confirming its stratigraphic attribution. The Middle Palaeolithic lithics at the site were first described as para-Charentian cultural facies following typological analyses. The revision of the earlier collection supplemented with the new material, using a technological approach, allow to identify two layers dominated by Levallois production followed by discoid production (Layers C8 and C6) surrounding an original assemblage (layer C7), characterised by a dominant Levallois production completed by three secondary production systems of equal importance, including discoid, SSDA and a Quina-like production. The faunal spectrum predominantly comprises an assemblage of Pleistocene large mammals, and biochronological studies corroborate the dates obtained.

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    Authors: Jacob, Jérémy; Reimer, Paula; Bard, Edouard; Bayliss, Alex; +27 Authors

    The IntCal09 and Marine09 radiocarbon calibration curves have been revised utilizing newly available and updated data sets from 14C measurements on tree rings, plant macrofossils, speleothems, corals, and foraminifera. The calibration curves were derived from the data using the random walk model (RWM) used to generate IntCal09 and Marine09, which has been revised to account for additional uncertainties and error structures. The new curves were ratified at the 21st International Radiocarbon conference in July 2012 and are available as Supplemental Material at www.radiocarbon.org. The database can be accessed at http://intcal.qub.ac.uk/intcal13/.

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    Radiocarbon
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    Radiocarbon
    Article . 2013 . Peer-reviewed
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      Radiocarbon
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      Radiocarbon
      Article . 2013 . Peer-reviewed
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    Authors: Fei Han; Jean-Jacques Bahain; Chun-Ru Liu; Gongming Yin;

    Abstract Several mathematical models have been suggested to describe uranium migration kinetics for ESR dating of fossil tooth. In the present study, different U-uptake models were used to calculate ages for fossil teeth from two open-air Paleolithic sites in Nihewan Basin – Donggutuo and Hougou and compared with independent age control of the sites. For Donggutuo site, the results show that the ages of three teeth calculated by EU and AU models were much younger than magnetostratigraphic age. At Hougou site, two teeth from the top of Nihewan lacustrine deposits give the consistent EU and AU ages within errors but younger than sediment OSL age. This study indicates that mathematical modeling could not always give convincing results for the open-air sites, which may experience dramatic hydrological variations and high erosion rates.

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    Quaternary Geochronology
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    Quaternary Geochronology
    Article . 2015 . Peer-reviewed
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      Quaternary Geochronology
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      Quaternary Geochronology
      Article . 2015 . Peer-reviewed
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  • image/svg+xml Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao Closed Access logo, derived from PLoS Open Access logo. This version with transparent background. http://commons.wikimedia.org/wiki/File:Closed_Access_logo_transparent.svg Jakob Voss, based on art designer at PLoS, modified by Wikipedia users Nina and Beao
    Authors: Rapp, Reinhard; Xu, V.; Zock, Michael; Sharoff, S.; +5 Authors

    This chapter describes several approaches of using comparable corpora beyond the area of MT for under-resourced languages, which is the primary focus of the ACCURAT project. Section 7.1, which is based on Rapp and Zock (Automatic dictionary expansion using non-parallel corpora. In: A. Fink, B. Lausen, W. Seidel, & A. Ultsch (Eds.) Advances in Data Analysis, Data Handling and Business Intelligence. Proceedings of the 32nd Annual Meeting of the GfKl, 2008. Springer, Heidelberg, 2010), addresses the task of creating resources for bilingual dictionaries using a seed lexicon; Sect. 7.2 (based on Rapp et al., Identifying word translations from comparable documents without a seed lexicon. Proceedings of LREC 2012, Istanbul, 2012) develops and evaluates a novel methodology of creating bilingual dictionaries without an initial lexicon. Section 7.3 proposes a novel system that can extract Chinese–Japanese parallel sentences from quasi-comparable and comparable corpora.

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    https://doi.org/10.1007/978-3-...
    Part of book or chapter of book . 2019 . Peer-reviewed
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    Part of book or chapter of book . 2019
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      https://doi.org/10.1007/978-3-...
      Part of book or chapter of book . 2019 . Peer-reviewed
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    Authors: Joël Rosato; Nelly Bonifaci; Zhiling Li; Roland Stamm;

    Spectral lines of hydrogen observed in a corona discharge are investigated. The corona discharge has been performed at the vicinity of a tip electrode under high voltage. The shape of the H-α and H-β lines is dominated by the Stark broadening due to the plasma microfield. Using a computer simulation method, we examine the sensitivity of the line shapes to the electron density. Our results indicate the possibility of a density diagnostic based on passive spectroscopy.

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    Journal of Physics : Conference Series
    Article . 2017 . Peer-reviewed
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    Other literature type . Conference object . 2016
    Hyper Article en Ligne; Hal-Diderot
    Other literature type . Article . 2017
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    Authors: Georges Clauzon; Paul Le Strat; Cédric Duvail; Damien Do Couto; +10 Authors

    The Roussillon Basin is a non-silled Miocene sedimentary basin filling a late Oligocene–early Miocene graben. The basin was intensively impacted by the 2 Messinian fluvial erosion, as evidenced in exposed sections, in seismic profiles and in deep boreholes drilled for hydrocarbon exploration. As the basin was open to the Mediterranean Sea, the huge drop in sea level at the peak of the Messinian Salinity Crisis is clearly recorded, along with the subsequent sudden marine reflooding and the resulting prograding sedimentary filling, particularly in Gilbert-type fan deltas. Here, the Messinian Erosional Surface (MES) is accurately mapped in a high-resolution document, which corrects the confusion resulting from the set of 1:50,000 scale regional maps. Aim of the 3D reconstruction of the MES is to modernize geological mapping, a crucial challenge for Mediterranean and peripheral areas. Thanks to a reliable chronostratigraphy provided by planktonic foraminifers, calcareous nannofossils, micro-and macro-mammal remains, paleomagnetism and a 10 Be cosmogenic nuclide-derived study, our reconstruction is one of the most comprehensive models of changes in sea level from 6 to 3 Ma. After the marine reflooding of the Mediterranean Basin at 5.46 Ma, the fluctuations in sea level recorded in the Roussillon Basin were forced by global changes. Following reflooding, the Prades large olistostrome collapsed prepared by the previous exhumation along the Canigou fault. The olistostrome is a good example of a local accident resulting from Messinian events. The exceptional changes in sea level at the peak of the Messinian Salinity Crisis deeply marked the Roussillon Basin, momentarily overprinting the Pyrenean orogenesis. Key words: Roussillon Basin – Messinian subaerial erosion –Zanclean sedimentary filling –Prades olistostrome. International audience

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    Marine and Petroleum Geology
    Article . 2015 . Peer-reviewed
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      Marine and Petroleum Geology
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Chersoni, Emmanuele; Santus, Enrico; Lenci, Alessandro; Blache, Philippe; +1 Authors

    Several studies on sentence processing suggest that the mental lexicon keeps track of the mutual expectations between words. Current DSMs, however, represent context words as separate features, thereby loosing important information for word expectations, such as word interrelations. In this paper, we present a DSM that addresses this issue by defining verb contexts as joint syntactic dependencies. We test our representation in a verb similarity task on two datasets, showing that joint contexts achieve performances comparable to single dependencies or even better. Moreover, they are able to overcome the data sparsity problem of joint feature spaces, in spite of the limited size of our training corpus. Comment: 5 pages

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    Authors: R. Ma; R. Ma; S. Sépulcre; L. Licari; +4 Authors

    Abstract. We have measured Cd/Ca ratios of several benthic foraminiferal species and studied benthic foraminiferal assemblages on two cores from the northern Indian Ocean (Arabian Sea and northern Bay of Bengal, BoB), in order to reconstruct variations in intermediate-water circulation and paleo-nutrient content since the last deglaciation. Intermediate water Cdw records estimated from the benthic Cd/Ca reflect past changes in surface productivity and/or intermediate–bottom-water ventilation. The benthic foraminiferal assemblages are consistent with the geochemical data. These results suggest that during the last deglaciation, Cdw variability was primarily driven by changes in intermediate-water properties, indicating an enhanced ventilation of intermediate–bottom water masses during both Heinrich Stadial 1 and the Younger Dryas (HS1 and YD, respectively). During the Holocene, however, surface primary productivity appears to have influenced Cdw more than intermediate water mass properties. This is evident during the early Holocene (from 10 to 6 cal ka) when benthic foraminiferal assemblages indicate that surface primary productivity was low, resulting in low intermediate-water Cdw at both sites. Then, from ∼ 5.2 to 2.4 cal ka, surface productivity increased markedly, causing a significant increase in the intermediate-water Cdw in the southeastern Arabian Sea and the northeastern BoB. The comparison of intermediate-water Cdw records with previous reconstructions of past Indian monsoon evolution during the Holocene suggests a direct control of intermediate-water Cdw by monsoon-induced changes in upper-water stratification and surface primary productivity. International audience

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    Climate of the Past (CP)
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    Authors: Pedro Cermeño; Carmen García-Comas; Alexandre Pohl; Simon Williams; +6 Authors

    21 pages, 3 figures, supplementary information https://doi.org/10.1038/s41586-022-04932-6.-- Data availability: Fossil diversity digitized data and those data downloaded from the Sepkoski’s Online Genus Database (http://strata.geology.wisc.edu/jack/) are provided as source data with this paper. Diversity data downloaded from the Ocean Biodiversity Information System (OBIS) database (www.obis.org) are also provided as source data with this paper. Source data are provided with this paper.-- Code availability: The coupled palaeogeographical–diversification model presented here uses input data of seafloor age distributions and palaeoenvironmental conditions from the siwill22/agegrid-0.1 v1-alpha palaeogeographical model and the cGENIE Earth system model, respectively. The code used to reconstruct seafloor age distributions from GPlates full-plate tectonic reconstructions is available at Zenodo (https://doi.org/10.5281/zenodo.3271360). The code for the version of the ‘muffin’ release of the cGENIE Earth system model used in this paper is tagged as v0.9.30, and is available at Zenodo (https://doi.org/10.5281/zenodo.6676435). Configuration files for the specific experiments presented in the paper can be found in the directory: genie-userconfigs/PUBS/published/Cermeno_et_al.2022. Details of the experiments, plus the command line needed to run each one, are given in the readme.txt file in that directory. The code for the muffingen boundary file generator, is available at Zenodo (https://doi.org/10.5281/zenodo.6676451). The code for the coupled palaeogeographical–diversification model is available at Zenodo (https://doi.org/10.5281/zenodo.6535496). The code is also available at GitHub (https://github.com/CarmenGarciaComas/INDITEK); this is the recommended mode of access as it will contain any updates and clarifications The fossil record of marine invertebrates has long fuelled the debate as to whether or not there are limits to global diversity in the sea1,2,3,4,5. Ecological theory states that, as diversity grows and ecological niches are filled, the strengthening of biological interactions imposes limits on diversity6,7. However, the extent to which biological interactions have constrained the growth of diversity over evolutionary time remains an open question1,2,3,4,5,8,9,10,11. Here we present a regional diversification model that reproduces the main Phanerozoic eon trends in the global diversity of marine invertebrates after imposing mass extinctions. We find that the dynamics of global diversity are best described by a diversification model that operates widely within the exponential growth regime of a logistic function. A spatially resolved analysis of the ratio of diversity to carrying capacity reveals that less than 2% of the global flooded continental area throughout the Phanerozoic exhibits diversity levels approaching ecological saturation. We attribute the overall increase in global diversity during the Late Mesozoic and Cenozoic eras to the development of diversity hotspots under prolonged conditions of Earth system stability and maximum continental fragmentation. We call this the ‘diversity hotspots hypothesis’, which we propose as a non-mutually exclusive alternative to the hypothesis that the Mesozoic marine revolution led this macroevolutionary trend12,13 This work was funded by research grant CGL2017-91489-EXP from the Spanish government. A.P. acknowledges funding from the European Union’s Horizon research and innovation programme under the Marie Skłodowska-Curie grant agreement no. 838373. S.W. was supported by NSFC grant no. 41972237 and ARC grant nos DP180102280 and DP200100966. M.J.B. acknowledges support through ERC Advanced Grant ‘Innovation’ (ERC 788203). P.C. and S.M.V. acknowledge support through grant no. CTM2017-87227-P. A.R. acknowledges NSF grant EAR-2121165, as well as support from the Heising–Simons Foundation. The Institut de Ciències del Mar (CSIC) received funding from the Spanish government through the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S) Peer reviewed

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    Nature
    Other literature type . Article . 2022 . Peer-reviewed
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    Nature
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    Authors: Trépied, Benoît; Muckle, Adrian;

    ABSTRACT For more than a century, from the 1870s to the 1980s, stockmen were important intermediaries and figures of power and influence in the construction, maintenance and renewal of the colonial order in New Caledonia. Social relations between Kanak and settlers working in the cattle ‘runs’ permitted a unique form of mobility spanning the frontier. The relations developed between chiefs and cattle farmers are central to the processes by which certain administrative chieftaincies emerged in the late‐nineteenth century, and by which Kanak entered the ‘political’ sphere in the second half of the twentieth century. With reference to the locality of Koné, this article traces the political alliances fashioned between Kanak stockmen and their employers in the context of colonisation, rebellion, evangelisation, post‐war political emancipation, local development and, finally, the struggle between supporters and opponents of independence in the 1980s.

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    Oceania
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    Authors: Thibaud Saos; Sophie Grégoire; Jean-Jacques Bahain; Thomas Higham; +11 Authors

    This paper presents new archaeological material and first dates on Upper Pleistocene layers at the site of La Crouzade cave (Gruissan, Aude, France). The site was first excavated by T. and P. Héléna at the beginning of the twentieth century, and the excavations were recently completed during three years (2016–2018) of systematic campaigns. We obtained dates from Middle Palaeolithic layers using two methods: AMS 14C dates were obtained from bone and charcoal, and combined ESR-U series dating was undertaken on horse teeth. Together, these methods allowed us to date this Mousterian sequence to 49,776–44805 cal BP for the deepest level (layer C8) and from 42,000 ± 3000 years BP for the top (layer C6). The Upper Palaeolithic layers are preserved only as patches in the actual excavation area, but a date was obtained from a piece of charcoal collected from a small hearth preserved in the first layer (C5) above Middle Palaeolithic deposits, which indicates an age similar to that of a modern human maxillary previously analysed and re-dated here from 36,014 to 34402 cal BP, confirming its stratigraphic attribution. The Middle Palaeolithic lithics at the site were first described as para-Charentian cultural facies following typological analyses. The revision of the earlier collection supplemented with the new material, using a technological approach, allow to identify two layers dominated by Levallois production followed by discoid production (Layers C8 and C6) surrounding an original assemblage (layer C7), characterised by a dominant Levallois production completed by three secondary production systems of equal importance, including discoid, SSDA and a Quina-like production. The faunal spectrum predominantly comprises an assemblage of Pleistocene large mammals, and biochronological studies corroborate the dates obtained.

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    Authors: Jacob, Jérémy; Reimer, Paula; Bard, Edouard; Bayliss, Alex; +27 Authors

    The IntCal09 and Marine09 radiocarbon calibration curves have been revised utilizing newly available and updated data sets from 14C measurements on tree rings, plant macrofossils, speleothems, corals, and foraminifera. The calibration curves were derived from the data using the random walk model (RWM) used to generate IntCal09 and Marine09, which has been revised to account for additional uncertainties and error structures. The new curves were ratified at the 21st International Radiocarbon conference in July 2012 and are available as Supplemental Material at www.radiocarbon.org. The database can be accessed at http://intcal.qub.ac.uk/intcal13/.

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    Radiocarbon
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    Radiocarbon
    Article . 2013 . Peer-reviewed
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      Radiocarbon
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      Radiocarbon
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    Authors: Fei Han; Jean-Jacques Bahain; Chun-Ru Liu; Gongming Yin;

    Abstract Several mathematical models have been suggested to describe uranium migration kinetics for ESR dating of fossil tooth. In the present study, different U-uptake models were used to calculate ages for fossil teeth from two open-air Paleolithic sites in Nihewan Basin – Donggutuo and Hougou and compared with independent age control of the sites. For Donggutuo site, the results show that the ages of three teeth calculated by EU and AU models were much younger than magnetostratigraphic age. At Hougou site, two teeth from the top of Nihewan lacustrine deposits give the consistent EU and AU ages within errors but younger than sediment OSL age. This study indicates that mathematical modeling could not always give convincing results for the open-air sites, which may experience dramatic hydrological variations and high erosion rates.

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    Quaternary Geochronology
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    Quaternary Geochronology
    Article . 2015 . Peer-reviewed
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      Quaternary Geochronology
      Article . 2015 . Peer-reviewed
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    Authors: Rapp, Reinhard; Xu, V.; Zock, Michael; Sharoff, S.; +5 Authors

    This chapter describes several approaches of using comparable corpora beyond the area of MT for under-resourced languages, which is the primary focus of the ACCURAT project. Section 7.1, which is based on Rapp and Zock (Automatic dictionary expansion using non-parallel corpora. In: A. Fink, B. Lausen, W. Seidel, & A. Ultsch (Eds.) Advances in Data Analysis, Data Handling and Business Intelligence. Proceedings of the 32nd Annual Meeting of the GfKl, 2008. Springer, Heidelberg, 2010), addresses the task of creating resources for bilingual dictionaries using a seed lexicon; Sect. 7.2 (based on Rapp et al., Identifying word translations from comparable documents without a seed lexicon. Proceedings of LREC 2012, Istanbul, 2012) develops and evaluates a novel methodology of creating bilingual dictionaries without an initial lexicon. Section 7.3 proposes a novel system that can extract Chinese–Japanese parallel sentences from quasi-comparable and comparable corpora.

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    https://doi.org/10.1007/978-3-...
    Part of book or chapter of book . 2019 . Peer-reviewed
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      https://doi.org/10.1007/978-3-...
      Part of book or chapter of book . 2019 . Peer-reviewed
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    Authors: Joël Rosato; Nelly Bonifaci; Zhiling Li; Roland Stamm;

    Spectral lines of hydrogen observed in a corona discharge are investigated. The corona discharge has been performed at the vicinity of a tip electrode under high voltage. The shape of the H-α and H-β lines is dominated by the Stark broadening due to the plasma microfield. Using a computer simulation method, we examine the sensitivity of the line shapes to the electron density. Our results indicate the possibility of a density diagnostic based on passive spectroscopy.

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    Journal of Physics : Conference Series
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    Authors: Georges Clauzon; Paul Le Strat; Cédric Duvail; Damien Do Couto; +10 Authors

    The Roussillon Basin is a non-silled Miocene sedimentary basin filling a late Oligocene–early Miocene graben. The basin was intensively impacted by the 2 Messinian fluvial erosion, as evidenced in exposed sections, in seismic profiles and in deep boreholes drilled for hydrocarbon exploration. As the basin was open to the Mediterranean Sea, the huge drop in sea level at the peak of the Messinian Salinity Crisis is clearly recorded, along with the subsequent sudden marine reflooding and the resulting prograding sedimentary filling, particularly in Gilbert-type fan deltas. Here, the Messinian Erosional Surface (MES) is accurately mapped in a high-resolution document, which corrects the confusion resulting from the set of 1:50,000 scale regional maps. Aim of the 3D reconstruction of the MES is to modernize geological mapping, a crucial challenge for Mediterranean and peripheral areas. Thanks to a reliable chronostratigraphy provided by planktonic foraminifers, calcareous nannofossils, micro-and macro-mammal remains, paleomagnetism and a 10 Be cosmogenic nuclide-derived study, our reconstruction is one of the most comprehensive models of changes in sea level from 6 to 3 Ma. After the marine reflooding of the Mediterranean Basin at 5.46 Ma, the fluctuations in sea level recorded in the Roussillon Basin were forced by global changes. Following reflooding, the Prades large olistostrome collapsed prepared by the previous exhumation along the Canigou fault. The olistostrome is a good example of a local accident resulting from Messinian events. The exceptional changes in sea level at the peak of the Messinian Salinity Crisis deeply marked the Roussillon Basin, momentarily overprinting the Pyrenean orogenesis. Key words: Roussillon Basin – Messinian subaerial erosion –Zanclean sedimentary filling –Prades olistostrome. International audience

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    Marine and Petroleum Geology
    Article . 2015 . Peer-reviewed
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      Marine and Petroleum Geology
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