James R. Bonelli

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—Previous observations about the stable nature of coral-rich assemblages from the Middle Devonian Hamilton Group have led some researchers to invoke the primacy of ecological controls in maintaining biofacies structure through time. However, few analyses have examined the degree to which recurring biofacies vary quantitatively, and none have assessed(More)
In Monmouth County, New Jersey, the Upper Cretaceous Navesink Formation is well-exposed along the banks of Big Brook at the Boundary Road Bridge and along the banks of Poricy Brook at Poricy Park on the Middletown-Linecroft Road. Field and laboratory investigations conducted at Hofstra University over the last four years have begun to elucidate the sequence(More)
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