The breakup of the L-chondrite parent body in the asteroid belt 466 million years (Ma) ago
still delivers almost a third of all meteorites falling on Earth. Our new extraterrestrial chromite …

The catastrophic disruption of the L chondrite parent body in the asteroid belt c. 470 Ma
initiated a prolonged meteorite bombardment of Earth that started in the Ordovician and …

Abstract The Middle Ordovician (Da**ian–middle Darriwilian)“orthoceratite limestone” is
documented in its traditional type area at Kinnekulle in the province of Västergötland in …

Abstract The Middle Ordovician conodont genera that are suitable for palaeoenvironmental
interpretations from the epicontinental Baltoscandian platform have been identified and …

More than a quarter of all meteorites falling on Earth today originate from the breakup of the
L-chondrite parent body (LCPB)∼ 470 Ma ago, the largest documented asteroid breakup in …

Hyoliths are a group of Palaeozoic fossils with calcareous shells whose affinities remain
controversial. As their shells were originally aragonitic, their fossils are usually coarsely …

Carbonate fluorapatite-filled millimeter-scale microsteinkerns are a key element of the
“Small Shelly Fossil”(SSF) fauna generally associated with the late Proterozoic–Cambrian …

A ca 20 m thick succession of upper Furongian (Cambrian Stage 10) through Middle
Ordovician (Darriwilian) strata exposed at Lanna, in the province of Närke, south-central …

Abstract The Komstad Limestone forms a distal part of the widespread 'orthoceratite
limestone'of the Baltoscandian continent. In this paper, we present an integrated conodont …

Under mellanordovicium täcktes paleokontinenten Baltica av ett grundhav och i det
temperade klimatet som rådde avsattes långsamt kallvattenkarbonater som kom att täcka …