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Micropaleontology
Study of microscopic fossils
Protists
Single-celled eukaryotic organisms
Protists types
Autotrophic (plant-like) and heterotrophic (animal-like)
Acritarchs
Organic marine microfossils (<100 μm), Proterozoic–Recent
Dinoflagellates
Organic aquatic microfossils (5–150 μm), Silurian–Recent
Coccolithophores
Calcite marine microfossils (<50 μm), Triassic–Recent
Diatoms
Silica aquatic microfossils (<200 μm), Jurassic–Recent
Radiolarians
Silica marine microfossils (0.03–1.5 mm), Cambrian–Recent
Foraminifera
Organic/agglutinated/calcareous marine microfossils (0.01–100 mm), Cambrian–Recent
Ostracods
Calcareous aquatic microfossils (1–10 mm), Cambrian–Recent
Conodonts
Phosphatic marine microfossils (0.1–5 mm), Cambrian–Triassic
Spores
Organic terrestrial microfossils (5 μm–4 mm), Devonian–Recent
Pollen
Organic terrestrial microfossils (5–200 μm), Devonian–Recent
Microfossils groups
Protists, multicelled organisms, plant parts
Ostracods
Small crustaceans with two valves
Ostracod shell
Calcareous carapace
Ostracod morphology
Bean-shaped with hinged valves
Ostracod habitat
Benthic (marine and freshwater) and pelagic (marine)
Freshwater ostracods
Thin, smooth shells
Marine benthic ostracods
Thick, ornamented shells
High-energy ostracods
Thick shells with ribs/spines
Infaunal ostracods
Elongated smooth shells
Pelagic ostracods
Rounded smooth shells
Foraminifera
Single-celled protozoans with shells (tests)
Foraminifera habitat
Benthic and planktonic
Foraminifera shell
Test
Foraminifera chambers
Added in spiral arrangement
Foraminifera aperture
Last chamber opening
Foramina
Pores for pseudopodia
Foraminifera test types
Organic, agglutinated, calcareous
Porcelaneous test
Translucent
Microgranular test
Common in Paleozoic
Hyaline test
Transparent
Foraminifera growth patterns
Planispiral, trochospiral, biserial, uniserial
Planktonic forams
Globular, porous, buoyant
Benthic forams
Flattened or elongated
Epifaunal forams
Feed on diatoms
Infaunal forams
Feed on organic matter and bacteria
Foraminifera environment
Controlled by temperature and salinity
Photic zone
0–200 m (light penetration zone)
Foraminifera uses
Paleoclimate, paleoceanography, biostratigraphy
Foraminifera evolution
Cambrian agglutinated → Silurian calcareous → Devonian multi-chambered → Jurassic planktonic
Diatoms
Silica microfossils used in environmental reconstruction
Diatom skeleton
Frustule (silica)
Diatom groups
Centric and pennate
Diatom analysis steps
Core sampling, dating, extraction, counting, identification
Diatom use
Paleoclimate and paleoenvironment reconstruction
Trace fossils
Evidence of organism activity
Ichnology
Study of trace fossils
Trace fossils definition
In situ records of behavior
Trace fossil types
Tracks, burrows, borings, coprolites
Ichnotaxa
Classification based on trace, not organism
Ichnogenus
Genus of trace fossil
Ichnospecies
Species of trace fossil
Trace fossil principles
Same organism produces different traces
Trace fossil principle
Same trace produced by different organisms
Trace fossil preservation
Varies with sediment
Trace fossil modification
Affected by environment
Burrowing reasons
Protection, feeding, respiration, reproduction
Burrowing methods
Compression, excavation, displacement
Cubichnia
Resting traces
Repichnia
Locomotion traces
Fodinichnia
Feeding traces
Domichnia
Dwelling traces
Pascichnia
Grazing traces
Agrichnia
Farming traces
Fugichnia
Escape traces
Praedichnia
Predation traces
Equilibrichnia
Equilibrium adjustment traces
Environmental controls
Energy, depth, salinity, nutrients, oxygen, substrate
Facies
Rock characteristics reflecting depositional environment
Ichnofacies
Trace fossil assemblage indicating environment
Ichnofacies importance
Behavior consistent through time
Bioturbation
Sediment disturbance by organisms
Bioturbation meaning
Indicates sedimentation rate and oxygen levels
No bioturbation
Rapid sedimentation or anoxic conditions