This document provides information about identifying and recognizing planktonic foraminifera. It notes that planktonic foraminifera lack additional skeletal structures found in benthic foraminifera, have a simple aperture, can permanently float or drift in the water column, and are very abundant in inner to outer neritic sediments. It also describes the wall textures of different planktonic foraminifera species and how their morphology has evolved over time, including developing elongate chamber extensions, becoming biserial, and muricae fusing.