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) et de spéciation du fer atteste d'une oscillation entre des conditions suboxiques et anoxiques au sein des domaines profonds du Bassin Vocontien, au cours de l'OAE 2. Les enrichissements faibles en éléments indicateurs de productivité primaire (P, Ni, Cu, Ba), suggèrent cependant que celle-ci fut relativement modeste pour ce bassin. Ces conditions appauvries en oxygène furent interrompues par une phase d'intense réoxygénation, appelée Plenus Cold Event (PCE), semblant correspondre à une chute de la pCO2 induite par le piégeage massif du CO2 au sein de la matière organique dans les sédiments et par une consommation accrue CO2 par altération continentale. Les valeurs d'enrichissements relatifs en Mo et en U indiquent, par ailleurs, un faible renouvellement des eaux profondes, confirmant le caractère semi-confiné du Bassin Vocontien à cette période et suggère une mise en place d'une stratification de la colonne d'eau. L'évolution du signal isotopique de l'azote dans les sédiments atteste de périodes d'intensification de la fixation de N2 atmosphérique par des bactéries diazotrophes, Cet évènement est caractérisé par la présence d'enregistrements sédimentaires présentant un contenu en matière organique élevé, à l'origine d'une large excursion positive du signal de ? 13 C à l'échelle globale. Des indices géochimiques et biologiques indiquent que ces enregistrements sédimentaires sont associés à une diminution de la quantité d'O2 dans les sédiments et la colonne d'eau ,
, lié à la pyrite, marquée par une large excursion négative, suppose un développement de conditions sulfidiques depuis les sédiments vers la limite avec la colonne d'eau, voire au sein de la colonne d'eau. La sulfato-réduction microbienne s'effectuant dans un système « ouvert » par rapport au réservoir de sulfates marin, il est proposé que celle-ci fût alimentée par un apport de soufre issu d'émissions d'origine volcanique, Ces conditions sulfidiques ont pu induire un recyclage du phosphore dans la colonne d'eau
développement de conditions appauvries en oxygène en favorisant la mise en place d'une stratification de la colonne d'eau. L'émission de CO2 et de soufre d'origine volcanique dans les océans, induisant une cascade de rétroactions positives affectant les cycles biogéochimiques, semble être l'élément déclencheur de la désoxygénation à l'échelle du Bassin Vocontien comme à l'échelle globale. Les bassins ayant enregistré les conditions de désoxygénation de la colonne d'eau les plus sévères, comme l'Atlantique Central ou les bassins profonds de l'Ouest-Téthys, sont caractérisés par un faible renouvellement des eaux profondes, mais également par des conditions de forte productivité primaire, associées à des apports de nutriments importants ,