The Quercy Phosphorites Formation in France is world famous for its Eocene to Miocene faunas, especially those from the upper Eocene to lower Oligocene, the richest of all. The latter particularly helped to understand the ‘Grande Coupure’, a dramatic faunal turnover event that occurred in Europe during the Eocene-Oligocene transition. Fossils from the Quercy Phosphorites were excavated from the middle 19th century until the early 20th century in a series of sites and became subsequently dispersed over several research institutions, while often losing the temporal and geographical information in the process. In this contribution, we provide an overview and reassess the taxonomy of these barely known collections housed in three Belgian institutions: the Université de Liège, KU Leuven, and the Royal Belgian Institute of Natural Sciences. We focus our efforts on the carnivorous mammals (Hyaenodonta and Carnivoramorpha) and assess the stratigraphic intervals covered by each collection. These fossils are derived from upper Eocene (Priabonian), lower Oligocene (Rupelian), and upper Oligocene (Chattian) deposits in the Quercy area. The richness of the three collections (e.g., the presence of numerous postcranial elements in the Liège collection), the presence of types and figured specimens in the Leuven collection, and some identified localities in the RBINS collection make these collections of great interest for further studies on systematics and the evolution of mammals around the ‘Grande Coupure’.
                                      
                                          
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                                                  RBINS Staff Publications 2021
                                                  
                                               
                                          
                                      
                                    
                              
                              
                                    
                                      
                                      The feeding activity and burrow ventilation by benthic invertebrates importantly affect the biodiversity and  functioning of seafloor sediments. Here we investigated how ocean acidification can modify these behavioural  activities in two common and abundant macrofaunal ecosystem engineering species in temperate continental  shelf communities: the white furrow shell Abra alba and the sand mason Lanice conchilega. Using time-lapse  imagery  and  sediment  porewater  hydraulic  signatures  we  show  that  both  species  adapt  their  behaviour  in  response to predicted future pH conditions (-0.3 units). During a three-week laboratory experiment, A. alba  reduced the duration per feeding event when suspension and deposit feeding (by 86 and 53%, respectively), and  almost completely ceased suspension feeding under reduced seawater pH in comparison to ambient seawater pH  (pH  ~  8.2).  This  behavioural  change  reduces  the  intake  of  low  pH  water  during  feeding  and  respiration.  L. conchilega increased its piston-pumping frequency by 30 and 52%, respectively, after one and two weeks of  exposure to future pH conditions (-0.3 units) relative to ambient conditions. This change in irrigation activity  suggests higher metabolic demands under low seawater pH, and also extended low water column pH conditions  deeper into the seafloor. Because the distribution of other populations depends on the physicochemical setting by  our focal species, we argue that the demonstrated behavioural plasticity will likely have cascading effects on  seafloor diversity and functioning, highlighting the complexity of how ocean acidification, and climate change in  general, will affect seafloor ecology.
                                      
                                          
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                                                  RBINS Staff Publications 2023