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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: Hartmut Egger; Udo Kreickemeier; Jens Wrona;

    AbstractThis paper sets up a two‐country model of offshoring with monopolistically competitive product and monopsonistically competitive labor markets. In our model, an incentive for offshoring exists even between symmetric countries, because shifting part of the production abroad reduces local labor demand and allows firms to more strongly execute their monopsonistic labor market power. However, offshoring between symmetric countries has negative welfare effects and therefore calls for policy intervention. In this context, we put forward the role of a common minimum wage and show that the introduction of a moderate minimum wage increases offshoring and reduces welfare. In contrast, a sizable minimum wage reduces offshoring and increases welfare. Beyond that, we also show that a sufficiently high common minimum wage cannot only eliminate offshoring but also inefficiencies in the resource allocation due to monopsonistic labor market distortions in closed economies.

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    SSRN Electronic Journal
    Article . 2024 . Peer-reviewed
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      SSRN Electronic Journal
      Article . 2024 . Peer-reviewed
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    Authors: Joely Marie Maak; Daniel Birgel; Joachim Reitner; Eberhard Gischler; +3 Authors

    AbstractMicrobial carbonates are common components of Quaternary tropical coral reefs. Previous studies revealed that sulfate-reducing bacteria trigger microbial carbonate precipitation in supposedly cryptic reef environments. Here, using petrography, lipid biomarker analysis, and stable isotope data, we aim to understand the formation mechanism of microbial carbonate enclosed in deep fore reef limestones from Mayotte and Mohéli, Comoro Islands, which differ from other reefal microbial carbonates in that they contain less microbial carbonate and are dominated by numerous sponges. To discern sponge-derived lipids from lipids enclosed in microbial carbonate, lipid biomarker inventories of diverse sponges from the Mayotte and Mohéli reef systems were examined. Abundant peloidal, laminated, and clotted textures point to a microbial origin of the authigenic carbonates, which is supported by ample amounts of mono-O-alkyl glycerol monoethers (MAGEs) and terminally branched fatty acids; both groups of compounds are attributed to sulfate-reducing bacteria. Sponges revealed a greater variety of alkyl chains in MAGEs, including new, previously unknown, mid-chain monomethyl- and dimethyl-branched MAGEs, suggesting a diverse community of sulfate reducers different from the sulfate-reducers favoring microbialite formation. Aside from biomarkers specific for sulfate-reducing bacteria, lipids attributed to demosponges (i.e., demospongic acids) are also present in some of the sponges and the reefal carbonates. Fatty acids attributed to demosponges show a higher diversity and a higher proportion in microbial carbonate compared to sponge tissue. Such pattern reflects significant taphonomic bias associated with the preservation of demospongic acids, with preservation apparently favored by carbonate authigenesis.

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    OceanRep; Facies
    Article . 2024 . 2023 . Peer-reviewed
    License: CC BY
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      OceanRep; Facies
      Article . 2024 . 2023 . Peer-reviewed
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    Authors: H. Tim Breitfeld; Juliane Hennig-Breitfeld; Gavin Anthony; Marcelle BouDagher-Fadel; +5 Authors
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    Marine and Petroleum Geology
    Article . 2023 . Peer-reviewed
    License: Elsevier TDM
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      Marine and Petroleum Geology
      Article . 2023 . 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/
    Authors: Feldberg, Kathrin; Hedenäs, Lars; Schmidt, Alexander R.;

    http://dx.doi.org/10.13039/501100001659 German Research Foundation

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    Palaeoworld
    Article . 2023 . Peer-reviewed
    License: Elsevier TDM
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      Palaeoworld
      Article . 2023 . 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/
    Authors: Gernot Arp; Yagmur Balmuk; Stephan Seppelt; Andreas Reimer;

    Ein temporärer Aufschluss im südlichen Niedersachsen ermöglichte die sedimentologische, geochemische und paläontologische Untersuchung eines 40.8 m mächtigen Toarcium-Profils, vom Top der Amaltheenton-, über die Posidonienschiefer- und Jurensismergel-, bis zum tieferen Teil der Opalinuston-Formation. Horizontierte Ammoniten- und Belemnitenfunde, Bivalvenassoziationen, sowie Daten aus benachbarten Profilen lassen für das Untere Toarcium eine weitgehend vollständige Abfolge von Ammoniten-Zonen und -Subzonen erkennen. Eine markante Schichtlücke an der Posidonienschiefer/Jurensismergel-Formationsgrenze umfasst wahrscheinlich die Semipolitum-Subzone sowie die Variabilis-und Thouarsense-Zone. Über einer kondensierten Dispansum-Zone folgt das höhere Ober-Toarcium mit einer vermutlich weitgehend vollständigen, allerdings nur punktuell direkt belegbaren, Zonen- und Subzonen-Abfolge. Eine dünne, stromatolithführende Kondensationslage ist nur für den Grenzbereich Pseudoradiosa- zu Mactra/Aalensis-Subzone erkennbar. Die Grenze Toarcium/Aalenium kann nur mittels Belemnitenfunden an einer weiteren dünnen Kondensationlage festgelegt werden. Erst wenige Meter darüber kann die Opalinum-Zone mittels schlecht erhaltener Ammoniten wahrscheinlich gemacht werden. Auf Grundlage von Diskontinuitäten, Lithofazies, Biofazies und Korrelationen mit Nachbarprofilen wird eine Unterteilung in Alloformationen, welche weitgehend den Formationen entsprechen, durchgeführt. Darauf aufbauend kann eine sequenzstratigraphische Interpretation bezüglich Transgressions-Regressions-Zyklen (T-R-Sequenzen) dritter Ordnung abgeleitet werden: Über dem regressiven höheren Teil der Alloformation 1 (Amaltheenton-Formation) mit einer maximalen Regressionsfläche (mrs) nahe seinem Top ist die T-R-Sequenz der Alloformation 2 (Posidonienschiefer Formation) entwickelt, mit einer maximalen Überflutungsfläche (mfs) am Übergang Falciferum/Commune-Subzone und nachfolgender regressiver Phase innerhalb der höheren Bifrons-Zone. Für die Commune-Subzone belegen eingeregelte Belemniten eine grundberührende Strömung aus südsüdwestlicher Richtung. Die nachfolgende maximale Regressionsfläche (mrs) liegt im Bereich der Bifrons/Variabilis-Zonengrenze. Die nächste Sequenz ist am untersuchten Profil nicht überliefert. Sie ist dagegen weiter östlich wie auch weiter westlich mit der transgressiven Dörnten-Subformation (Variabilis- und Thouarsense-Zone) erhalten geblieben. Die regressive Phase (Fallaciosum-Subzone) fehlt allerdings auch dort, angezeigt durch eine markante Sequenzgrenze mit Erosionsrelief an der Basis der Dispansum-Zone. Die Alloformation 3 (Jurensismergel- und tiefste Teile der Opalinuston-Formation) repräsentiert eine weitere T-R-Sequenz mit maximaler Überflutungsfläche (Basis Mactra/Aalensis-Subzone) und einer etwas längeren regressive Phase (Aalensis-Subzone). Die folgende maximale Regressionsfläche stellt die Grenze zur Alloformation 4 (Hauptteil der Opalinuston-Formation) dar, nachfolgend wieder mit kürzerer transgressiver Phase (Pseudolotharingicum-Subzone), Kondensationshorizont und längerer regressiver Phase (Opalinum-Zone). Diese sequenzstratigraphischen Interpretationen stehen weitgehend in Einklang mit bisherigen Untersuchungen aus Nord- und Süddeutschland. Marginale zeitliche Abweichungen von maximalen Transgressions- oder Regressionsflächen spiegeln wahrscheinlich Effekte durch höhere Subsidenz bei variablen Sedimentationsraten im norddeutschen Becken wider. Für die am Untersuchungsort nur lückenhaft aufgeschlossene Opalinuston-Formation bedarf es weiterer Untersuchungen an vollständigen Kernprofilen. A temporary outcrop in southern Lower Saxony permitted the sedimentological, geochemical and palaeontological investigation of a 40.8 m thick Toarcian section, from the top of the Amaltheenton Formation, through the Posidonienschiefer and Jurensismergel Formations, to lower parts of the Opalinuston Formation. Bed by bed collected ammonites and belemnites, bivalve associations, as well as data from neighbouring sections indicate a largely complete sequence of ammonite zones and subzones for the Lower Toarcian. A prominent stratigraphic gap at the Posidonienschiefer/Jurensismergel Formation boundary probably comprises the Semipolitum Subzone as well as the Variabilis and Thouarsense Zones. Above a condensed Dispansum Zone follows the higher Upper Toarcian with a presumably largely complete sequence of zones and subzones, although direct evidence for this is only sporadic. However, a thin condensed bed with stromatolite crusts is recognisable at the boundary Pseudoradiosa to Mactra/Aalensis Subzone. The Toarcian/Aalenian boundary can only be drawn on basis of belemnite finds at another thin condensed bed. Only a few metres above, the Opalinum Zone is evident by ammonite findings. Based on discontinuities, lithofacies, biofacies and correlations with neighbouring sections, a subdivision into alloformations, which largely correspond to formations, is applied. Based on that, a sequence stratigraphic interpretation with respect to third order transgression-regression cycles (T-R sequences) can be inferred: Above the regressive upper parts alloformation 1 (Amaltheenton Formation) with a maximum regression surface (mrs) near its top, the T-R sequence of the alloformation 2 (Posidonienschiefer Formation) is developed, with a maximum flooding surface (mfs) at the transition Falciferum/Commune Subzone and the regressive phase within the later Bifrons Zone. For the Commune Subzone, belemnite alignment indicates a seawater bottom current from SSE. The following maximum regression surface (mrs) lies near the Bifrons/Variabilis Zone boundary. The next sequence is not preserved at the studied location, but is preserved further East as well as further West, represented by the transgressive Dörnten Member (Variabilis and Thouarsense Zone). However, the regressive phase (Fallaciosum Subzone) is also missing there, indicated by a prominent sequence boundary with erosional relief at the base of the Dispansum Zone. The following alloformation 3 (Jurensismergel Formation and lowermost parts Opalinuston Formation) represents another T-R sequence with a maximum transgressive surface (base Mactra/Aalensis subzone) and a slightly thicker regressive Aalensis Subzone. The following maximum regression surface represents the boundary to alloformation 4 (major parts of Opalinuston Formation), followed again by a short transgressive phase (Pseudolotharingicum Subzone), condensation horizon and a longer regressive phase (Opalinum Zone). These sequence stratigraphic interpretations are largely consistent with previous investigations in Northern and Southern Germany. Minor deviations in the timely position of maximum flooding and regression surfaces likely reflect effects of a higher subsidence at variable sedimentation rate in the North German Basin. With respect to the, at the site of investigation, incompletely exposed Opalinuston Formation, further studies on complete drill core sections are required.

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    Zitteliana
    Article . 2023
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    ZENODO; Zitteliana
    Article . 2023 . Peer-reviewed
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      Zitteliana
      Article . 2023
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      ZENODO; Zitteliana
      Article . 2023 . Peer-reviewed
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    Authors: Cristina Quintas-Soriano; Mario Torralba; María García-Martín; Tobias Plieninger;

    Abstract Rural abandonment is a significant process in the Mediterranean region, posing sustainability challenges for rural and urban areas. Although there is an increase in studies focusing on the ecological implications and impacts of land abandonment and the role of rewilding, there is a knowledge gap in the study of the socio-cultural dimension of abandonment from the local perspective, even though it is crucial for land management decision. This study focuses on a case study in Western Spain, where a social survey was used to assess the perceptions of local communities regarding land abandonment and their implication on nature’s contributions to people and quality of life. A survey campaign was administered in the case study region during the summer of 2020, collecting 205 face-to-face surveys. The results show that local communities overall have a negative reaction toward rural abandonment. In addition, local respondents recognize how traditional agriculture is the main source for maintaining nature’s contributions to human well-being. Additionally, four groups of narratives toward rural abandonment were identified representing clusters of respondents with different motivations and interpretations of rural abandonment. This paper calls for understanding better the perceptions, values, and motivations toward rural abandonment and how their outcomes can be used as input for landscape management. Our results indicate that the local population perceives that the loss of rural livelihoods may entail serious environmental and societal problems, as locals are forced to abandon their rural-associated ways of life and migrate to urban areas. Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659 Universität Kassel 501100012687

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    Regional Environmental Change
    Article . 2023 . Peer-reviewed
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      Regional Environmental Change
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    Authors: Gabriele, Russo; Annemieke, Milks; Dirk, Leder; Tim, Koddenberg; +6 Authors

    Abstract During the Upper Paleolithic, lions become an important theme in Paleolithic art and are more frequent in anthropogenic faunal assemblages. However, the relationship between hominins and lions in earlier periods is poorly known and primarily interpreted as interspecies competition. Here we present new evidence for Neanderthal-cave lion interactions during the Middle Paleolithic. We report new evidence of hunting lesions on the 48,000 old cave lion skeleton found at Siegsdorf (Germany) that attest to the earliest direct instance of a large predator kill in human history. A comparative analysis of a partial puncture to a rib suggests that the fatal stab was delivered with a wooden thrusting spear. We also present the discovery of distal lion phalanges at least 190,000 old from Einhornhöhle (Germany), representing the earliest example of the use of cave lion skin by Neanderthals in Central Europe. Our study provides novel evidence on a new dimension of Neanderthal behavioral complexity. Niedersächsisches Ministerium für Wissenschaft und Kultur http://dx.doi.org/10.13039/501100010570 Volkswagen Foundation http://dx.doi.org/10.13039/501100001663 Eberhard Karls Universität Tübingen 501100002345 Ramón y Cajal Spanish fallowiship

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    Scientific Reports
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      Scientific Reports
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    In diesem Beitrag beschreiben wir, wie die Forschungsdatenplattform Discuss Data um einen Bereich ("Communityspace") für die Digital Humanities (DH) erweitert wird. Dazu ergründen wir die Spezifika dieses Forschungsbereichs für einen entsprechenden Communityspace in Discuss Data und hinterfragen auch kritisch, wie erfolgreich bisherige Ansätze der Plattform Discuss Data im Aufbau der Community des Space für die "Osteuropa, Südkaukasus und Zentralasien" Forschung verlaufen sind und wie diese Erfahrungen bei dem Aufbau eines neuen Communityspace einbezogen werden können. Dies betrifft auch Kernbestandteile, wie die Vernetzungskomponenten und die Möglichkeit für Diskussionen über Daten auf der Plattform.

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    Authors: Civitelli, M; Ravidà, DCG; Borrelli, M; Criniti, S; +1 Authors

    http://dx.doi.org/10.13039/501100007069 Università della Calabria

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    Authors: Schatz, Merle; Schmidt, Birgit;

    Interoperable and shared European digital research infrastructures (DRI) shall enable ENLIGHT researchers to better collaborate, share their research data, and develop new ideas. Connecting DRIs is a complex process for all actors involved. This report brings together examples of current work tasks and challenges, using examples from DARIAH, CLARIN, NBIS (the Swedish node in ELIXIR). The goal is to provide insights into the diversity of the task related to connecting DRIs. 

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    Authors: Hartmut Egger; Udo Kreickemeier; Jens Wrona;

    AbstractThis paper sets up a two‐country model of offshoring with monopolistically competitive product and monopsonistically competitive labor markets. In our model, an incentive for offshoring exists even between symmetric countries, because shifting part of the production abroad reduces local labor demand and allows firms to more strongly execute their monopsonistic labor market power. However, offshoring between symmetric countries has negative welfare effects and therefore calls for policy intervention. In this context, we put forward the role of a common minimum wage and show that the introduction of a moderate minimum wage increases offshoring and reduces welfare. In contrast, a sizable minimum wage reduces offshoring and increases welfare. Beyond that, we also show that a sufficiently high common minimum wage cannot only eliminate offshoring but also inefficiencies in the resource allocation due to monopsonistic labor market distortions in closed economies.

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    SSRN Electronic Journal
    Article . 2024 . Peer-reviewed
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      SSRN Electronic Journal
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    Authors: Joely Marie Maak; Daniel Birgel; Joachim Reitner; Eberhard Gischler; +3 Authors

    AbstractMicrobial carbonates are common components of Quaternary tropical coral reefs. Previous studies revealed that sulfate-reducing bacteria trigger microbial carbonate precipitation in supposedly cryptic reef environments. Here, using petrography, lipid biomarker analysis, and stable isotope data, we aim to understand the formation mechanism of microbial carbonate enclosed in deep fore reef limestones from Mayotte and Mohéli, Comoro Islands, which differ from other reefal microbial carbonates in that they contain less microbial carbonate and are dominated by numerous sponges. To discern sponge-derived lipids from lipids enclosed in microbial carbonate, lipid biomarker inventories of diverse sponges from the Mayotte and Mohéli reef systems were examined. Abundant peloidal, laminated, and clotted textures point to a microbial origin of the authigenic carbonates, which is supported by ample amounts of mono-O-alkyl glycerol monoethers (MAGEs) and terminally branched fatty acids; both groups of compounds are attributed to sulfate-reducing bacteria. Sponges revealed a greater variety of alkyl chains in MAGEs, including new, previously unknown, mid-chain monomethyl- and dimethyl-branched MAGEs, suggesting a diverse community of sulfate reducers different from the sulfate-reducers favoring microbialite formation. Aside from biomarkers specific for sulfate-reducing bacteria, lipids attributed to demosponges (i.e., demospongic acids) are also present in some of the sponges and the reefal carbonates. Fatty acids attributed to demosponges show a higher diversity and a higher proportion in microbial carbonate compared to sponge tissue. Such pattern reflects significant taphonomic bias associated with the preservation of demospongic acids, with preservation apparently favored by carbonate authigenesis.

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    OceanRep; Facies
    Article . 2024 . 2023 . Peer-reviewed
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      OceanRep; Facies
      Article . 2024 . 2023 . Peer-reviewed
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    Authors: H. Tim Breitfeld; Juliane Hennig-Breitfeld; Gavin Anthony; Marcelle BouDagher-Fadel; +5 Authors
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    Marine and Petroleum Geology
    Article . 2023 . Peer-reviewed
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      Marine and Petroleum Geology
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    Authors: Feldberg, Kathrin; Hedenäs, Lars; Schmidt, Alexander R.;

    http://dx.doi.org/10.13039/501100001659 German Research Foundation

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    Palaeoworld
    Article . 2023 . Peer-reviewed
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      Palaeoworld
      Article . 2023 . Peer-reviewed
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    Authors: Gernot Arp; Yagmur Balmuk; Stephan Seppelt; Andreas Reimer;

    Ein temporärer Aufschluss im südlichen Niedersachsen ermöglichte die sedimentologische, geochemische und paläontologische Untersuchung eines 40.8 m mächtigen Toarcium-Profils, vom Top der Amaltheenton-, über die Posidonienschiefer- und Jurensismergel-, bis zum tieferen Teil der Opalinuston-Formation. Horizontierte Ammoniten- und Belemnitenfunde, Bivalvenassoziationen, sowie Daten aus benachbarten Profilen lassen für das Untere Toarcium eine weitgehend vollständige Abfolge von Ammoniten-Zonen und -Subzonen erkennen. Eine markante Schichtlücke an der Posidonienschiefer/Jurensismergel-Formationsgrenze umfasst wahrscheinlich die Semipolitum-Subzone sowie die Variabilis-und Thouarsense-Zone. Über einer kondensierten Dispansum-Zone folgt das höhere Ober-Toarcium mit einer vermutlich weitgehend vollständigen, allerdings nur punktuell direkt belegbaren, Zonen- und Subzonen-Abfolge. Eine dünne, stromatolithführende Kondensationslage ist nur für den Grenzbereich Pseudoradiosa- zu Mactra/Aalensis-Subzone erkennbar. Die Grenze Toarcium/Aalenium kann nur mittels Belemnitenfunden an einer weiteren dünnen Kondensationlage festgelegt werden. Erst wenige Meter darüber kann die Opalinum-Zone mittels schlecht erhaltener Ammoniten wahrscheinlich gemacht werden. Auf Grundlage von Diskontinuitäten, Lithofazies, Biofazies und Korrelationen mit Nachbarprofilen wird eine Unterteilung in Alloformationen, welche weitgehend den Formationen entsprechen, durchgeführt. Darauf aufbauend kann eine sequenzstratigraphische Interpretation bezüglich Transgressions-Regressions-Zyklen (T-R-Sequenzen) dritter Ordnung abgeleitet werden: Über dem regressiven höheren Teil der Alloformation 1 (Amaltheenton-Formation) mit einer maximalen Regressionsfläche (mrs) nahe seinem Top ist die T-R-Sequenz der Alloformation 2 (Posidonienschiefer Formation) entwickelt, mit einer maximalen Überflutungsfläche (mfs) am Übergang Falciferum/Commune-Subzone und nachfolgender regressiver Phase innerhalb der höheren Bifrons-Zone. Für die Commune-Subzone belegen eingeregelte Belemniten eine grundberührende Strömung aus südsüdwestlicher Richtung. Die nachfolgende maximale Regressionsfläche (mrs) liegt im Bereich der Bifrons/Variabilis-Zonengrenze. Die nächste Sequenz ist am untersuchten Profil nicht überliefert. Sie ist dagegen weiter östlich wie auch weiter westlich mit der transgressiven Dörnten-Subformation (Variabilis- und Thouarsense-Zone) erhalten geblieben. Die regressive Phase (Fallaciosum-Subzone) fehlt allerdings auch dort, angezeigt durch eine markante Sequenzgrenze mit Erosionsrelief an der Basis der Dispansum-Zone. Die Alloformation 3 (Jurensismergel- und tiefste Teile der Opalinuston-Formation) repräsentiert eine weitere T-R-Sequenz mit maximaler Überflutungsfläche (Basis Mactra/Aalensis-Subzone) und einer etwas längeren regressive Phase (Aalensis-Subzone). Die folgende maximale Regressionsfläche stellt die Grenze zur Alloformation 4 (Hauptteil der Opalinuston-Formation) dar, nachfolgend wieder mit kürzerer transgressiver Phase (Pseudolotharingicum-Subzone), Kondensationshorizont und längerer regressiver Phase (Opalinum-Zone). Diese sequenzstratigraphischen Interpretationen stehen weitgehend in Einklang mit bisherigen Untersuchungen aus Nord- und Süddeutschland. Marginale zeitliche Abweichungen von maximalen Transgressions- oder Regressionsflächen spiegeln wahrscheinlich Effekte durch höhere Subsidenz bei variablen Sedimentationsraten im norddeutschen Becken wider. Für die am Untersuchungsort nur lückenhaft aufgeschlossene Opalinuston-Formation bedarf es weiterer Untersuchungen an vollständigen Kernprofilen. A temporary outcrop in southern Lower Saxony permitted the sedimentological, geochemical and palaeontological investigation of a 40.8 m thick Toarcian section, from the top of the Amaltheenton Formation, through the Posidonienschiefer and Jurensismergel Formations, to lower parts of the Opalinuston Formation. Bed by bed collected ammonites and belemnites, bivalve associations, as well as data from neighbouring sections indicate a largely complete sequence of ammonite zones and subzones for the Lower Toarcian. A prominent stratigraphic gap at the Posidonienschiefer/Jurensismergel Formation boundary probably comprises the Semipolitum Subzone as well as the Variabilis and Thouarsense Zones. Above a condensed Dispansum Zone follows the higher Upper Toarcian with a presumably largely complete sequence of zones and subzones, although direct evidence for this is only sporadic. However, a thin condensed bed with stromatolite crusts is recognisable at the boundary Pseudoradiosa to Mactra/Aalensis Subzone. The Toarcian/Aalenian boundary can only be drawn on basis of belemnite finds at another thin condensed bed. Only a few metres above, the Opalinum Zone is evident by ammonite findings. Based on discontinuities, lithofacies, biofacies and correlations with neighbouring sections, a subdivision into alloformations, which largely correspond to formations, is applied. Based on that, a sequence stratigraphic interpretation with respect to third order transgression-regression cycles (T-R sequences) can be inferred: Above the regressive upper parts alloformation 1 (Amaltheenton Formation) with a maximum regression surface (mrs) near its top, the T-R sequence of the alloformation 2 (Posidonienschiefer Formation) is developed, with a maximum flooding surface (mfs) at the transition Falciferum/Commune Subzone and the regressive phase within the later Bifrons Zone. For the Commune Subzone, belemnite alignment indicates a seawater bottom current from SSE. The following maximum regression surface (mrs) lies near the Bifrons/Variabilis Zone boundary. The next sequence is not preserved at the studied location, but is preserved further East as well as further West, represented by the transgressive Dörnten Member (Variabilis and Thouarsense Zone). However, the regressive phase (Fallaciosum Subzone) is also missing there, indicated by a prominent sequence boundary with erosional relief at the base of the Dispansum Zone. The following alloformation 3 (Jurensismergel Formation and lowermost parts Opalinuston Formation) represents another T-R sequence with a maximum transgressive surface (base Mactra/Aalensis subzone) and a slightly thicker regressive Aalensis Subzone. The following maximum regression surface represents the boundary to alloformation 4 (major parts of Opalinuston Formation), followed again by a short transgressive phase (Pseudolotharingicum Subzone), condensation horizon and a longer regressive phase (Opalinum Zone). These sequence stratigraphic interpretations are largely consistent with previous investigations in Northern and Southern Germany. Minor deviations in the timely position of maximum flooding and regression surfaces likely reflect effects of a higher subsidence at variable sedimentation rate in the North German Basin. With respect to the, at the site of investigation, incompletely exposed Opalinuston Formation, further studies on complete drill core sections are required.

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    Zitteliana
    Article . 2023
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    ZENODO; Zitteliana
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      Zitteliana
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      ZENODO; Zitteliana
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    Authors: Cristina Quintas-Soriano; Mario Torralba; María García-Martín; Tobias Plieninger;

    Abstract Rural abandonment is a significant process in the Mediterranean region, posing sustainability challenges for rural and urban areas. Although there is an increase in studies focusing on the ecological implications and impacts of land abandonment and the role of rewilding, there is a knowledge gap in the study of the socio-cultural dimension of abandonment from the local perspective, even though it is crucial for land management decision. This study focuses on a case study in Western Spain, where a social survey was used to assess the perceptions of local communities regarding land abandonment and their implication on nature’s contributions to people and quality of life. A survey campaign was administered in the case study region during the summer of 2020, collecting 205 face-to-face surveys. The results show that local communities overall have a negative reaction toward rural abandonment. In addition, local respondents recognize how traditional agriculture is the main source for maintaining nature’s contributions to human well-being. Additionally, four groups of narratives toward rural abandonment were identified representing clusters of respondents with different motivations and interpretations of rural abandonment. This paper calls for understanding better the perceptions, values, and motivations toward rural abandonment and how their outcomes can be used as input for landscape management. Our results indicate that the local population perceives that the loss of rural livelihoods may entail serious environmental and societal problems, as locals are forced to abandon their rural-associated ways of life and migrate to urban areas. Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659 Universität Kassel 501100012687

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    Regional Environmental Change
    Article . 2023 . Peer-reviewed
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      Regional Environmental Change
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    Authors: Gabriele, Russo; Annemieke, Milks; Dirk, Leder; Tim, Koddenberg; +6 Authors

    Abstract During the Upper Paleolithic, lions become an important theme in Paleolithic art and are more frequent in anthropogenic faunal assemblages. However, the relationship between hominins and lions in earlier periods is poorly known and primarily interpreted as interspecies competition. Here we present new evidence for Neanderthal-cave lion interactions during the Middle Paleolithic. We report new evidence of hunting lesions on the 48,000 old cave lion skeleton found at Siegsdorf (Germany) that attest to the earliest direct instance of a large predator kill in human history. A comparative analysis of a partial puncture to a rib suggests that the fatal stab was delivered with a wooden thrusting spear. We also present the discovery of distal lion phalanges at least 190,000 old from Einhornhöhle (Germany), representing the earliest example of the use of cave lion skin by Neanderthals in Central Europe. Our study provides novel evidence on a new dimension of Neanderthal behavioral complexity. Niedersächsisches Ministerium für Wissenschaft und Kultur http://dx.doi.org/10.13039/501100010570 Volkswagen Foundation http://dx.doi.org/10.13039/501100001663 Eberhard Karls Universität Tübingen 501100002345 Ramón y Cajal Spanish fallowiship

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    Scientific Reports
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      Scientific Reports
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    In diesem Beitrag beschreiben wir, wie die Forschungsdatenplattform Discuss Data um einen Bereich ("Communityspace") für die Digital Humanities (DH) erweitert wird. Dazu ergründen wir die Spezifika dieses Forschungsbereichs für einen entsprechenden Communityspace in Discuss Data und hinterfragen auch kritisch, wie erfolgreich bisherige Ansätze der Plattform Discuss Data im Aufbau der Community des Space für die "Osteuropa, Südkaukasus und Zentralasien" Forschung verlaufen sind und wie diese Erfahrungen bei dem Aufbau eines neuen Communityspace einbezogen werden können. Dies betrifft auch Kernbestandteile, wie die Vernetzungskomponenten und die Möglichkeit für Diskussionen über Daten auf der Plattform.

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    Authors: Civitelli, M; Ravidà, DCG; Borrelli, M; Criniti, S; +1 Authors

    http://dx.doi.org/10.13039/501100007069 Università della Calabria

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    Authors: Schatz, Merle; Schmidt, Birgit;

    Interoperable and shared European digital research infrastructures (DRI) shall enable ENLIGHT researchers to better collaborate, share their research data, and develop new ideas. Connecting DRIs is a complex process for all actors involved. This report brings together examples of current work tasks and challenges, using examples from DARIAH, CLARIN, NBIS (the Swedish node in ELIXIR). The goal is to provide insights into the diversity of the task related to connecting DRIs. 

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