Microfossil sampling benthic foraminiferans from the mudstone accumulated inside this 4-5 million year old Tresus pajaroanus clam. Benthic Foraminiferans are microscopic Protists that live on or in the the bottom sediments and are usually marine. Typically Forams are not well-preserved in sandstone here in the Purisima Formation. However, the fine mud and silt sediments that accumulated inside fossil clams such as this one often have a higher percentage of Forams preserved in them. Eastern Pacific Pliocene foraminifera are not well-studied and hopefully this project will add to our understanding of local environmental conditions and allow us to place the Purisima formation here within the larger biochronological framework.
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