• Adamastor – an ocean that never existed? 

      Konopasek, Jiri; Cavalcante, Carolina; Fossen, Haakon; Janoušek, Vojtěch (Journal article; Peer reviewed, 2020)
      Existing models of tectonic evolution of the Neoproterozoic orogenic system rimming the shores of the South Atlantic Ocean (the Araçuaí–Ribeira–Congo and Dom Feliciano–Kaoko–Gariep belts) interpret the belts as subduction-related ...
    • Clinoform systems: Review and dynamic classification scheme for shorelines, subaqueous deltas, shelf edges and continental margins 

      Patruno, Strefano; Helland-Hansen, William (Peer reviewed; Journal article, 2018-10)
      Clinoforms are inclined and normally basinward-dipping horizons developed over a range of spatial and temporal scales in both siliciclastic and carbonatic systems. The study of clinoform successions underpins sequence ...
    • Geochemical characterization of ophiolites in the Alpine-Himalayan Orogenic Belt: Magmatically and tectonically diverse evolution of the Mesozoic Neotethyan oceanic crust 

      Furnes, Harald; Dilek, Yildirim; Zhao, Guochun; Safonova, Inna; Santosh, M. (Journal article; Peer reviewed, 2020)
      Ophiolites are important archives of oceanic crust development and preservation in the rock record, and the Alpine-Himalayan Orogenic Belt (AHOB) is one of the most comprehensive ophiolite depositories in earth’s history. ...
    • Pollen-based climate reconstruction techniques for late Quaternary studies 

      Chevalier, Manuel; Davis, Basil A. S.; Heiri, Olivier; Seppä, Heikki; Chase, Brian M; Gajewski, Konrad; Lacourse, Terri; Telford, Richard; Finsinger, Walter; Guiot, Joël; Kühl, Norbert; Maezumi, S. Yoshi; Tipton, John R.; Carter, Vachel A.; Brussel, Thomas; Phelps, Leanne N.; Dawson, Andria; Zanon, Marco; Vallé, Francesca; Nolan, Connor; Mauri, Achille; de Vernal, Anne; Izumi, Kenji; Holmström, Lasse; Marsicek, Jeremiah; Goring, Simon; Sommer, Philipp S.; Chaput, Michelle; Kupriyanov, Dimitry (Journal article; Peer reviewed, 2020)
      Fossil pollen records are well-established indicators of past vegetation changes. The prevalence of pollen across environmental settings including lakes, wetlands, and marine sediments, has made palynology one of the most ...