The 'Orsten'-More than a Cambrian Konservat-Lagerstätte yielding exceptional preservation

In several areas of southern Sweden, limestone nodules, locally called Orsten occur within bituminous alum shales. These shales and nodules were deposited under dysoxic conditions at the bottom of what was most likely a shallow sea during the late Middle to Upper Cambrian (ca. 500 million years ago)...

Полное описание

Библиографические подробности
Главные авторы: Maas, A, Braun, A, Dong, X, Donoghue, P, Müller, K, Olempska, E, Repetski, J, Siveter, D, Stein, M, Waloszek, D
Формат: Journal article
Язык:English
Опубликовано: 2006