Our knowledge
of dinosaur evolution is based on a series of snapshots provided by the fossil
record, with a handful of key regions providing the lion’s share of information
for any particular time period. This relies on serendipity – rocks of the right
age and type need to be preserved in a way where they are accessible for
collection – and the distribution of these deposits is essentially random, due
to numerous geological processes acting to different extents in different areas
at different times. For example, our most detailed insights on the last
dinosaurs currently come from the western USA and Canada, whereas presently our
information on the earliest dinosaurs is confined to Argentina and Brazil.
Southern
Africa provides an important piece in this puzzle, with a series of sandstone
and mudstone deposits laid down on broad river floodplains, that were laid down
at a time when dinosaurs were first starting their rise to numerical and
ecological dominance. These environments became more arid through time,
culminating in vast dune seas, where dinosaur fossils could still be found.
This series of rocks is referred to as the Stormberg Group in South Africa and
reveals not only the dinosaurs but also the other members of a series of
terrestrial faunas that lived during the Late Triassic and Early Jurassic,
spanning a period when several pulses of extinction rocked the world at the
Triassic/Jurassic boundary. The Stormberg Group has been (and continues to be)
the focus of much attention and has yielded some of the best-known African
dinosaurs, which are often known from abundant and beautiful material. These
include the ornithischians Heterodontosaurus
and Lesothosaurus, the theropods Dracovenator and Coelophysis, and (most abundantly) the sauropodomorphs, including Antetonitrus, Massospondylus, Pulanesaura
and many others.
Adjacent
regions of southern Africa, including Botswana, Lesotho, Zambia and Zimbabwe, have
similar sedimentary series that are thought to correlate with those in South
Africa, but for various reasons these deposits are have been less thoroughly
explored. Nevertheless, some important material is known from these areas, with
rich localities in Lesotho (which have supplied beautiful early mammal and Lesothosaurus material, as well as dinosaur
footprints) and Zimbabwe. Many sites are known in Zimbabwe, with well-known
taxa such as Coelophysis and Massospondylus known from the south of
the country, while the early sauropod Vulcanodon
was found on the shores of Lake Kariba on its northern border. Several field
crews have worked on sites in the south of Zimbabwe more recently, finding new
and important material, but the potentially rich dinosaur sites around the
shores of Lake Kariba have not been prospected by palaeontologsts since the
time of Vulcanodon’s discovery in 1969.
More
recently, a small band of dedicated amateur palaeontologists and geologists,
including local safari camp owner Steve Edwards and geologist Tim Broderick,
have had their eyes to the ground along the shores of Lake Kariba and have found
interesting new material of their own. Steve and Tim mentioned this material to
various dinosaur specialists around the world, including my colleague Jonah
Choiniere (based at the Evolutionary Studies Institute in Johannesburg) and I. The
presence of Vulcanodon, and other
Early Jurassic dinosaurs elsewhere in Zimbabwe, as well as the exciting news
that new material was being found, suggested to Jonah and I that a trip to area
would be fruitful and exciting. After months of background research, building
new contacts with colleagues in Zimbabwe, and raising the money, Jonah was able
to organise an expedition to the Lake Kariba area, in which I was lucky enough
to participate, along with several other Zimbabwean and South African
colleagues. So, on the 5th January 2017 Jonah, his postdoc Pia Viglietti,
our joint PhD student Kimi Chapelle and I left Johannesburg, bound for Harare …
No comments:
Post a Comment
Please leave your comments below...