Spreite, meaning leaf-blade in German is a stacked, curved, layered structure that is characteristic of certain trace fossils. They are formed by invertebrate organisms tunnelingback and forth through sediment in search of food. The organism movesperpendicularly just enough at the start of each back-and-forth pass so that it avoids reworking a previously tunneled area, thereby ensuring that it only makes feeding passes through fresh, unworked sediment. Two types of spreiten are generally recognized. Protrusive spreiten result from movement of the organism away from its burrow entrance, whereas retrusive spreiten result from movement towards the burrow entrance. Vertical burrows with retrusive spreiten are also referred to as "escape burrows", as they represent attempts by the organism during periods of high sedimentation to prevent the burrow entrance from being buried, and at the same time keep the bottom of the burrow at the same distance from the sediment-water interface. In essence, the organism "escapes" from being buried too deeply by progressively tunneling upward, thereby leaving behind it a stacked vertical succession of concave-side-up spreite. Diplocraterion is the classic example of a vertical burrow with spreite, whereas Rhizocorallium is an example of a horizontal burrow with spreite. Spreiten differ from menisci, which are flat to slightly curved, back-filling structures found in some tubular burrows. Menisci are formed when the organism packs sediment, and sometimes fecal material as well, behind itself as it moves through the burrow. Because spreiten and menisci represent different behaviors, the distinction between spreiten and meniscate burrows is an important criterion for the identification of certain ichnotaxa. For example, generally parallel-sided, elongate, horizontal burrows with menisci are typically assigned to the Muensteriaichnospecies, whereas similar burrows with spreite will generally be assigned to the Rhizocorallium ichnogenus.
