Abstract In this paper, we trace the saga of the rocks and fossils discovered along Stevenson Road, northern Malawi. Fish and bivalves discovered along the road were proclaimed the first fossils of Central Africa. In the late nineteenth and early twentieth centuries, they became a large part of the ‘Tanganyika Problem’, the notion of whether a Jurassic incursion of the sea left fossils in what is now Malawi and relict marine invertebrates in Lake Tanganyika. Later studies clarified both the geology and zoology of the region, but no more informative fossils were found in Malawi until 2016 when a specimen of Eunotosaurus was discovered by a herdsman in the original nineteenth century fossil locality. He presented the fossil to the Cultural and Museum Centre Karonga, the public face of geoheritage in Malawi. That specimen constrains the upper age limit of the site to approximately 259 Ma (Late Permian). The Tanganyika Problem is now largely of historical interest, yet in a more current multidisciplinary context – the timing and mechanisms of the evolutionary transition of clades from the marine realm into freshwater biomes open new questions about historical biogeography in a geological context.

Abstract The jigsaw-puzzle fit of South America and Africa is an icon of plate tectonics and continental drift. Fieldwork in Angola since 2002 allows the correlation of onshore outcrops and offshore geophysical and well-core data in the context of rift, sag, salt, and post-salt drift phases of the opening of the central South Atlantic. These outcrops, ranging in age from >130 Ma to <71 Ma, record Early Cretaceous outpouring of the Etendeka–Paraná Large Igneous Province (Bero Volcanic Complex) and rifting, followed by continental carbonate and siliciclastic deposition (Tumbalunda Formation) during the sagging of the nascent central South Atlantic basin. By the Aptian, evaporation of sea water resulted in thick salt deposits (Bambata Formation), terminated by seafloor spreading. The Equatorial Atlantic Gateway began opening by the early Late Cretaceous (100 Ma) and allowed flow of currents between the North and South Atlantic, creating environmental conditions that heralded the introduction of marine reptiles. These dramatic outcrops are a unique element of geoheritage because they arguably comprise the most complete terrestrially exposed geological record of the puzzle-like icon of continental drift.

ABSTRACT Outcrops of Late Cretaceous Gulf Series strata (Woodbine, Eagle Ford, and Austin) in the Dallas area expose middle Cenomanian to the early Campanian (96 to ˜ 83 Ma) rocks, which are well known in the subsurface of the oil-rich East Texas Basin. Together with the underlying Comanche Series and overlying younger Gulf Series, this set of strata provides a record of the last 50 million years of the Cretaceous. Although both marine and terrestrial vertebrates are known in this interval, the Late Cretaceous record is primarily marine. On this field trip, sites are visited that have yielded sharks, bony fish, turtles, dinosaurs, crocodiles, pterosaurs, mammals, long- and short-necked plesiosaurs, and a classic record of mosasaur evolution.

Abstract The fossil record of lorisiforms in Asia is currently restricted to specimens recovered from a half-dozen localities of Miocene age (13 Ma to 7 Ma) in the Siwalik Group of northern Pakistan and in related deposits of India. More than one lorisid taxon is represented in the Pakistan material, but Nycticeboides simpsoni Jacobs, 1981 is currently the only named species. A partial skeleton of Nycticeboides , although poorly preserved, possesses diagnostic lorisid synapomorphies of the auditory region and the vertebral column. The fact that Nycticeboides was a small animal is important for understanding its ecology. A primate frugivore with the M 1 dimensions of Nycticeboides should have a body weight of only about 500 g according to commonly-used regression statistics. However, if Nycticeboides was mostly insectivorous, and its molar teeth scaled to body size in the manner characteristic of highly insectivorous primates and non-zalambdodont insectivores, then it may have weighed much less than this estimate.