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all geography including DSDP/ODP Sites and Legs
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
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Availability
Boney Springs Formation
ALBERT C. KOCH’S MISSOURIUM AND THE DEBATE OVER THE CONTEMPORANEITY OF HUMANS AND THE PLEISTOCENE MEGAFAUNA OF NORTH AMERICA Available to Purchase
C. W. BEEHLER’S COLLECTION OF VERTEBRATE FOSSILS: A LOST LEGACY Available to Purchase
The ‘other’ Glasgow Boys: the rise and fall of a school of palaeobotany Available to Purchase
Abstract With its long-standing coal industry working the measures of the Scottish central belt, fossil plants have long been known in Scotland. The earliest significant work dealing with Scottish palaeontology, David Ure’s The History of Rutherglen and East-Kilbride (David Niven, Glasgow) had been published in 1793, with its plates of Equisetum , ferns and bark impressions. But, as in Yorkshire and Lancashire, it was not until the industrial revolution’s increased exposure of fossils was matched by the advent of the ‘new European botany’ (which, in part, grew from substantial improvements in the optics for microscopy) that fossil plant study began in earnest in Scotland. In 1959 John Walton reflected on palaeobotany in Britain at the end of the 19th century, as ‘awakening from a long sleep’. In Glasgow, this awakening centred on the university’s Botany Department, and the development of the study of fossil plants closely parallels the growth of this department as a whole for much of its time. In the same city during this period a collective of artists called the ‘Glasgow Boys’ were pushing the boundaries of representational painting. With Frederick Bower’s own cohort of palaeobotanical ‘Glasgow Boys’ (David Gwynne-Vaughan and William Lang) facilitating the work of Robert Kidston, a veritable ‘School of Palaeobotany’ existed in the university at this time. John Walton himself was also destined to serve an unusual, but critical, later role in the preservation of Kidston’s work.
THE OCCURRENCE OF BONE MODIFICATION FEATURES IN THE CARAPACE AND PLASTRON OF THE EXTANT RED-EARED SLIDER TRACHEMYS SCRIPTA ELEGANS (WIED-NEUWIED, 1839): IMPLICATIONS FOR PALEOECOLOGICAL ANALYSES OF FOSSIL TURTLE ASSEMBLAGES Available to Purchase
Evaporites—a selected bibliography Available to Purchase
Holocene barrier-island geology and morphodynamics of the Maryland and Virginia open-ocean coasts: Fenwick, Assateague, Chincoteague, Wallops, Cedar, and Parramore Islands Available to Purchase
Abstract This four-day field trip will include 21 field stops along a 105-km reach of Maryland’s and Virginia’s barrier-island coast along the Delmarva Peninsula. Along the way, we will cover aspects of barrier-island and nearshore geology and of barrier-island and backbarrier marsh process-response morphodynamic systems in two hydrodynamic settings: (1) the wave-dominated Assateague Island along the northern Delmarva Peninsula and (2) the mixed-energy Virginia barrier islands along the southern Delmarva Peninsula. We will also examine anthropogenic impacts on barrier-island systems at Ocean City Inlet, Maryland, and the National Aeronautics and Space Administration’s (NASA) Wallops Island, Virginia.