Recent field studies on Upper Silurian stratigraphy and paleontology in the
Inner Mongolia Autonomous Region:(for short Inner Mongalia) near Bater Obo
(=Bateaobao) resulted in the discovery of a small continental island with
fossil invertebrates preserved as encrusters (stromatoporoids and corals) a
ttached directly to a rocky shore surface and buried by silty clay mud. The
Bater island (named herein) is 610 m x 200 m in size and composed of Ordov
ician igneous rock (diorite), Limestone strata dating from the Ludlow Epoch
(about 420 Ma) surround the island and dip away from the igneous core in a
radial pattern. The encrusting fossils occur on the sheltered (south and s
outheast) side of the island, whereas the north side was exposed to stronge
r wave activity based on a basal conglomerate unit composed of diorite boul
ders. This is the first record of an ancient island in China and the first
report worldwide of stromatoporoids as members of a rocky-shore community.
The island clearly shows distinct windward and leeward deposits comparable
to geologically younger islands from the Mesozoic and Cenozoic outside Chin
a.