Fossils in thin section
In limestones, most grains are pieces of organisms. Shape, size, wall structure and how the grain goes extinct under crossed polars tell you which group it came from, and that tells you what kind of rock and environment you're looking at.
Quick tips
- A grain that goes extinct all at once as a single crystal, often with a dusty mesh texture: echinoderm (crinoid) plate.
- A thin, curved shell ending in a hook ("shepherd's crook") with sweeping extinction: trilobite.
- A spar-filled mold with only the outline left: originally aragonite, usually a mollusc.
- Multiple small chambers in a row or coil, under about 1 mm: foraminifera.
- Tiny two-valved shells with overlapping edges: ostracods.
Groups
Foraminifera
Brachiopods
Molluscs: bivalves
Molluscs: gastropods
Molluscs: cephalopods
Echinoderms (crinoids, echinoids)
Bryozoans
Corals
Trilobites
Ostracods
Sponges and spicules
Calcareous algae
Stromatolites and stromatoporoidsno open-licensed photoRadiolariansno open-licensed photoCalcareous nannoplankton
BarnaclesOverview plates




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Sources
Rygel & Quinton, Sedimentary Geology 9.7: Fossils in Thin Section · SEPM Strata: Skeletal Grains · Rygel & Quinton, Sedimentary Geology 9.5: Microfossils