Temperature and Salinity historical data collections covering the time period 1900-2013/2014 were created for each European marginal sea (Arctic Sea, Baltic Sea, Black Sea, North Sea, North Atlantic Ocean, and Mediterranean Sea) within the framework of SeaDataNet2 Project and they are available as ODV collections through a web catalog (https://www.seadatanet.org/Products/Aggregated-datasets). Two versions have been published and they represent a snapshot of the SeaDataNet database content at two different times: V1.1 (January 2014) and V2 (March 2015). A Quality Control Strategy (QCS) was developped and continuously refined in order to improve the quality of the database content and create the best data products. The QCS consists of four main phases: 1) data harvesting from the data infrastructure; 2) file and parameter aggregation; 3) secondary quality check analysis; 4)correction of data anomalies. The approach is iterative to facilitate the upgrade of the database content and it allows a versioning of data products. Regional temperature and salinity monthly climatologies have been produced from V1.1 historical data collections and they are also available (https://www.seadatanet.org/Products/Climatologies). Within the new SeaDataCloud Project the release of updated historical data collections and new climatologies is planned. SeaDataCloud novelties are the introduction of decadal climatologies at various resolutions, the development of climatologies for the Global Ocean and a task dedicated to new data products, like Mixed Layer Depth climatologies, Ocean Heat Content estimates, coastal climatologies from HF radar data. All SeaDataCloud products are available through a dedicated web catalogue together with their relative Digital Object Identifier (DOI) and Product Information Document (PIDoc) containing all specifications about product’s generation, quality assessment and technical details to facilitate users’ uptake. The presentation will briefly overview the existing SeaDataNet products and introduce the SeaDataCloud products’ plan, but the main focus will be on the first release (February 2018) of SeaDataCloud Temperature and Salinity historical data collections, spanning the time period 1900-2017, their characteristics in terms of space-time data distribution and their usability.
Located in
Library
/
RBINS Staff Publications 2018
The Paleogene Period can be considered the cradle of modern marine and terrestrial ecosystems (e.g. Krug et al., 2009; Field et al,. 2018). After global catastrophe at the K-Pg boundary, life recovered and repopulated marine and terrestrial ecosystems (Vellekoop et al., 2017; Lowery et al., 2018; Lowery et al., 2019; Vellekoop et al., 2020), eventually heralding the establishment of the rich and diverse modern marine and terrestrial ecosystems (Krug et al., 2009; Field et al., 2018). It has been suggested the crucial biotic evolution and overturn during the Paleogene was at least partly driven by the climatic evolution across this time interval (e.g. Widlansky et al., 2021). For example, the PETM (56 Ma) likely was key in reshaping the biosphere (Smith et al., 2020). During this hyperthermal, the first representatives of modern mammal orders (e.g., primates, artiodactyls, perissodactyls) suddenly spread over all northern continents, while marine ecosystems are characterized by marked extinctions, radiations and migrations (Gibbs et al., 2012; Speijer et al., 2012). Nevertheless, the evolutionary importance of other warming pulses (e.g., Eocene Thermal Maximum 2 or ETM-2) or the gradual climate trends towards the EECO remains unclear for most fossil groups. For northwestern Europe, terrestrial faunas appear to have been almost consistently in a dynamic state across this time interval, strongly influenced by dispersal events. In contrast to the PETM, the exact timing and paleogeographic conditions remain poorly constrained for post-PETM warming pulses, as only tentative chronological correlation with the Paleogene global temperature curves are established. Therefore, we have initiated a new collaborative project, aimed at creating (1) a better chronostratigraphic framework of Paleogene bioevents among vertebrates, by detailed study of marine and terrestrial strata containing, or interfingering with, vertebrate-rich beds in NW Europe, and (2) generating a better understanding the role of climate change on biotic evolution and overturns during the Early Paleogene, from both a marine and terrestrial perspective.
Located in
Library
/
RBINS Staff Publications 2022 OA
The Quercy Phosphorites are a set of Eocene-Oligocene deposits from South-West France that yielded numerous vertebrate fossils, including amphibians, mostly as isolated bones. However, in 1873, several exceptional amphibian specimens were discovered, with the external surface of the unmineralized tissues preserved, and were commonly referred as “mummies”. In the 19th century, they were described without any knowledge of their internal anatomy. Since 2012, we have started scanning these “mummies”, revealing the preserved internal soft tissues and articulated skeleton. A first specimen was attributed in 2013 to Thaumastosaurus gezei and we here present our results from the tomography of a second “mummified” anuran, previously identified as Bufo servatus. The tomography showed a preserved articulated skeleton, and its osteological characteristics are similar to the first scanned anuran “mummy”, representing different ontogenetic stages. Both are now both attributed to Thaumastosaurus servatus nov. comb. The new anatomical information is used to assess the affinities of T. servatus, which appears to belong to the Pyxicephalidae, an African anuran clade. Thaumastosaurus thus represents both the oldest occurrence of this clade in the fossil record and its first occurrence outside of Africa. Its presence in Europe highlights a faunistic exchange with Africa during the Eocene, also documented for several clade of squamates. The presence of this African herpetofauna in Europe might be linked to the warmer climate during the Eocene. However, most of this herpetofauna, including Thaumastosaurus, disappeared from the region around an extinction event (named the “Grande Coupure”) that took place around the Eocene/Oligocene transition (~34 Ma).
Located in
Library
/
RBINS Staff Publications 2021
