Based on Merleau-Pontys’s philosophy of flesh, this paper outlines possibilities for organisational practices towards sustainability development. In order to elucidate these en-fleshed practices, the paper begins by presenting Merleau-Ponty’s phenomenology of the body and perception as well as his ontology of ‘flesh’. In particular, flesh is interpreted as elemental ‘carnality’ and formative medium. As such, it is processed through sensual and reflexive doubling as a reversibility and chiasm of the sentient and the sensible. This understanding opens for the path to (...) a post-dualistic, transformative approach towards processes of post-dualistic ‘wild being and ‘inter-be(com)ing’ in organisations. These concepts of Flesh are related to affect and imagination as well as organization and sustainability. The paper then offers some practical and political as well as research implications and concludes with some final perspectives on possible enfleshed inter-practices of sustainability. (shrink)

Die stratigraphischen Einheiten, durch welche heute die Erdgeschichte untergliedert wird, haben eine unterschiedliche und zum Teil recht komplexe Entstehungsgeschichte, wie hier am Beispiel des Keupers gezeigt werden soll. Das Wort ‘Keuper’ geht auf einen volkstümlichen Namen für bunte Tongesteine im Raum Coburg zurück. In den geologischen Sprachgebrauch wird es 1822 durch Leopold von Buch eingeführt, der es noch als Gesteinsnamen verwendet und die entsprechenden Schichten dem Buntsandstein zuweist. Die richtige Einstufung dieser Schichten über dem Muschelkalk gelang erstmals Ludwig Hausmann (...) und Peter Merian um 1820. Doch erst nachdem in den nachfolgenden Jahren deren Ergebnisse durch die Arbeit etlicher anderer Forscher bestätigt wurden, fand die neue, bis dahin unbenannte Formation aus bunten Mergeln und Sandsteinen breite Anerkennung. Als stratigraphischer Begriff, der auch Sandsteine und Gips umfaßt, wird die Bezeichnung Keuper erstmals von Friedrich Hoffmann im Jahre 1823 verwendet und von Christian Keferstein 1824 in die Literatur eingeführt. Eine wichtige Rolle spielten die Arbeit an den ersten geologischen Übersichtskarten Deutschlands und die Aufnahme der neuen Formation in die erste internationale Formationstabelle durch Keferstein . Mit der Integration des Keupers in die neue Formation ‘Trias’ durch Friedrich August von Alberti 1834 bekommt diese Einheit ihren seither festen Platz in der Stratigraphie.Geologic time is commonly subdivided by a set of stratigraphic terms, which all have their individual and sometimes complex histories. ‘Keuper’, now used as a stratigraphical term for the Upper Triassic, originated from a popular rock name of the Coburg area in southern Germany. The term ‘Keuper’, though still as a rock name, was first introduced into geological usage by Leopold von Buch in 1822, when he designated varicoloured marls and claystones, of what he thought to be Bunter Sandstein, as ‘Keuper’. In a stratigraphical sense, the term ‘Keuper-Formation’ was coined by Friedrich Hoffmann in 1823, who was the first to include sandstones and gypsum rocks with this notion. A year later it was introduced into the literature by Christian Keferstein. At this time, the existence of a distinct formation between Muschelkalk and Lias was already accepted by a number of geologists, though it had not yet been named. This ‘new’ formation has formerly been confused with Buntsandstein and even Carboniferous deposits by various authors until it was set into its right position by Ludwig Hausmann and Peter Merian in 1820. In the following years, the work of several geologists confirmed their results and led to general acceptance of the Keuper Formation as a separate entity. An important impetus came from the compilation of the first small-scale geological maps of Germany edited by Keferstein in the early 1820s, and from his international stratigraphical table , which already included the ‘Keuper-Formation’ as an integral part. In 1834, Friedrich August von Alberti included the ‘Keuper’ as part of the new Formation ‘Trias’ and thus defined its place in modern stratigraphy. (shrink)