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How Ammonite Causes

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Ammonite taxa often occur in narrow time ranges, arguably making them the best index fossils to determine the ages of strata of certain time intervals (Callomon, 2003). The fossil remnants of ammonites act as the major basis for the identification of Jurassic and Cretaceous strata in the Sverdrup Basin, reinforced by the presence of bivalves, dinoflagellates, and foraminifera (Galloway et al., 2013). While macrofossils such as ammonites are used to define every stage of the Jurassic and Cretaceous periods in the Sverdrup Basin, detailed chronostratigraphy is limited by the rare occurrence of ammonite fauna (Callomon, 2003). This may be due to the colder climate conditions of the Arctic Boreal Sea relative to the subtropical conditions of the

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