The change from a warm, ice-free greenhouse world to the glacial Antarctic icehouse
occurred during the latest Eocene–earliest Oligocene. Prior to this, during the Early–Middle …

The phytogeographic distribution of Cainozoic ferns is reported based upon a critical re-
appraisal of the macrofossil and mesofossil record also taking account of evidence from a …

Fossil wood is abundant in Cretaceous and early Tertiary sediments of the northern Antarctic
Peninsula region. The wood represents the remains of vegetation that once grew in high …

A high-resolution record of Eocene paleo-temperature variation is preserved within the high
southern latitude, marine shelf succession of the La Meseta Formation on Seymour Island …

Aptian to Pliocene time-series of X-ray fluorescence data from the Antarctic Peninsula are
used to assess the degree of chemical weathering and maturity of sediments deposited …

The Eocene of Seymour Island contains the only association of Cenozoic plants and land
vertebrates known from anywhere in Antarctica and lies at about latitude 63° south. The late …

• Premise of the study: Eocene caldera‐lake beds at Laguna del Hunco (LH, ca. 52.2 Ma)
and Río Pichileufú (RP, ca. 47.7 Ma) in Argentine Patagonia provide copious information …

Abundant and well‐preserved marine macrofossils on Seymour Island, Antarctica, provide a
valuable resource to establish paleoenvironmental conditions at high southern latitudes …

This paper evaluates whether 1) protoplatyrrhines could have migrated to South America via
Antarctica, and 2) the floating island model is a plausible transoceanic mode of dispersal for …

Fossil wood is abundant throughout the Cretaceous and Tertiary sequences of the northern
Antarctic Peninsula region. The fossil wood represents the remains of the vegetation that …