Fig. 2: Stratigraphy of the Esplugafreda sedimentary record.
From: Substantial continental temperature rise over the Paleocene-Eocene Thermal Maximum in the Pyrenees
a Synthetic lithostratigraphy and soil carbonate δ13C isotope profile of the Paleocene–Eocene interval (after Payros et al.30, modified from Pujalte et al.28) with (b) a field photo of the Esplugafreda and Claret Formation members in the western part of the Esplugafreda sector (from Pujalte et al.28).
