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Questions and Answers
Match the following levels of hierarchical classification:
Match the following levels of hierarchical classification:
Kingdom = Second highest taxonomic rank below Domain. Class = A taxonomic rank below Phylum and above Order. Family = A taxonomic rank below Order and above Genus. Order = A taxonomic rank below Class and above Family.
Match the following terms related to fossils with their descriptions:
Match the following terms related to fossils with their descriptions:
Fossil = Any object providing evidence of prehistoric life. Taphonomy = Study of changes between an organism’s death and fossil discovery. Paleoecology = The study of fossilized organisms, their life, and environment. Biomarker = Chemical signatures indicating past life.
Match the fossil types with their correct description:
Match the fossil types with their correct description:
Physical Remains = Actual shells, bones, or hard parts of an organism. Mineral Replacements = Original material replaced by minerals. Biological Impressions = Fossil records, such as tracks, trails, and burrows. Chemical Signatures = Distinctive substances, such as biomarkers, indicating past life.
Match the phrase with its level in the classification of life:
Match the phrase with its level in the classification of life:
Match the fossil preservation mode with its information retention:
Match the fossil preservation mode with its information retention:
Match the type of fossil with its description:
Match the type of fossil with its description:
Match the fossilization process with its description:
Match the fossilization process with its description:
Match the mineral with the conditions under which it commonly replaces fossils:
Match the mineral with the conditions under which it commonly replaces fossils:
Match the biogenic structure with its description:
Match the biogenic structure with its description:
Match the fossil type with its dimensional representation:
Match the fossil type with its dimensional representation:
Match the process with its example:
Match the process with its example:
Match the fossil with its primary environment:
Match the fossil with its primary environment:
Match the fossil type with the feature preserved:
Match the fossil type with the feature preserved:
Match the following preservation methods with their corresponding descriptions:
Match the following preservation methods with their corresponding descriptions:
Match the following minerals with the organism group that commonly uses them for hard parts:
Match the following minerals with the organism group that commonly uses them for hard parts:
Match the following altered hard part processes with their descriptions:
Match the following altered hard part processes with their descriptions:
Match the following fossil types to whether they are hard or soft parts:
Match the following fossil types to whether they are hard or soft parts:
Match each preservation type with the presence of alteration:
Match each preservation type with the presence of alteration:
Match the example mineral with the correct formula:
Match the example mineral with the correct formula:
Match the organism with the type of preservation:
Match the organism with the type of preservation:
Match the correct era with the preservation example:
Match the correct era with the preservation example:
Match the characteristic of a good index fossil with its description:
Match the characteristic of a good index fossil with its description:
Match the time period with the appearance of new predators.
Match the time period with the appearance of new predators.
Match the cephalopod adaptation with its function:
Match the cephalopod adaptation with its function:
Match the shell shape with its description:
Match the shell shape with its description:
Match the shell parameter formula to its effect.
Match the shell parameter formula to its effect.
Match the type of foraminifera with its shell type:
Match the type of foraminifera with its shell type:
Match the chambered shell solution with its description:
Match the chambered shell solution with its description:
Match the planktonic foraminifera characteristics:
Match the planktonic foraminifera characteristics:
Match the benthic foraminifera characteristics:
Match the benthic foraminifera characteristics:
Match the time period to the events:
Match the time period to the events:
Match the following algae types with their description:
Match the following algae types with their description:
Match the following benefits to why endosymbionts are helpful to foraminifera:
Match the following benefits to why endosymbionts are helpful to foraminifera:
Match the type of foraminifera shell wall with its description:
Match the type of foraminifera shell wall with its description:
Match the foraminifera group with its time period:
Match the foraminifera group with its time period:
Match the foraminifera group with what type of test they have:
Match the foraminifera group with what type of test they have:
Match the foraminifera group with its key features
Match the foraminifera group with its key features
Match the foraminifera group with its environmental niche
Match the foraminifera group with its environmental niche
Match the time period with foraminifera’s test type:
Match the time period with foraminifera’s test type:
Match that term with it’s meaning:
Match that term with it’s meaning:
Match those group with its key features.
Match those group with its key features.
Match the following processes of biostratinomy with their descriptions:
Match the following processes of biostratinomy with their descriptions:
Match the descriptions with the types of fossil transportation:
Match the descriptions with the types of fossil transportation:
Match the sedimentologic factors with their effects on organisms:
Match the sedimentologic factors with their effects on organisms:
Match the metabolic factors with their effects on marine life:
Match the metabolic factors with their effects on marine life:
Match the descriptions with the types of substrate consistency:
Match the descriptions with the types of substrate consistency:
Match the following cephalopod structures with their functions:
Match the following cephalopod structures with their functions:
Match the descriptions with the layers of a molluscan shell:
Match the descriptions with the layers of a molluscan shell:
Match the descriptions with the external anatomical features of a nautilus shell:
Match the descriptions with the external anatomical features of a nautilus shell:
Match the cephalopod ornamentation types with their function:
Match the cephalopod ornamentation types with their function:
Match the terms related to cephalopod sutures with their definitions:
Match the terms related to cephalopod sutures with their definitions:
Match the cephalopod subclasses with their key features:
Match the cephalopod subclasses with their key features:
Match the preservation types with their characteristics in nautiloids:
Match the preservation types with their characteristics in nautiloids:
Match the following orders of nautiloidea with their features:
Match the following orders of nautiloidea with their features:
Match the cephalopod groups with their biostratigraphic importance:
Match the cephalopod groups with their biostratigraphic importance:
Flashcards
Hierarchical Classification
Hierarchical Classification
A system organizing life from broad (Domain) to specific (Species).
Taphonomy
Taphonomy
The study of changes after an organism dies until it's found as a fossil.
Paleoecology
Paleoecology
Study of fossilized organisms, their lives, and environments.
Fossil
Fossil
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Unaltered Hard Parts
Unaltered Hard Parts
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Unaltered soft parts
Unaltered soft parts
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Altered soft parts
Altered soft parts
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Preservation methods for soft parts
Preservation methods for soft parts
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Anoxia
Anoxia
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Obrution
Obrution
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Fossil Lagerstätten
Fossil Lagerstätten
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Recrystallization
Recrystallization
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Carbonization
Carbonization
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Fossil Replacement
Fossil Replacement
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Dolomite
Dolomite
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Leached Fossils
Leached Fossils
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Steinkern (Core)
Steinkern (Core)
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Stromatolites
Stromatolites
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Thrombolites
Thrombolites
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Trace Fossils
Trace Fossils
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Mold
Mold
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Photosynthesis Benefit
Photosynthesis Benefit
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Photosynthesis & Calcification
Photosynthesis & Calcification
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Waste Removal by Symbionts
Waste Removal by Symbionts
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Agglutinated Test
Agglutinated Test
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Porcelaneous Test
Porcelaneous Test
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Hyaline Test
Hyaline Test
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Allogromiida
Allogromiida
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Textulariida
Textulariida
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Fusulinina
Fusulinina
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Globigerinida
Globigerinida
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Coprolites
Coprolites
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Biomarkers
Biomarkers
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Biostratinomy
Biostratinomy
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Disarticulation
Disarticulation
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Abrasion
Abrasion
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Reorientation
Reorientation
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Limiting Factors
Limiting Factors
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Epifauna
Epifauna
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Infauna
Infauna
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Turbulence
Turbulence
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Turbidity
Turbidity
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Siphuncle
Siphuncle
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Suture Line
Suture Line
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Phragmocone
Phragmocone
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Qualities of Good Index Fossils
Qualities of Good Index Fossils
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Timeline of Pelagic Predation
Timeline of Pelagic Predation
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Endocones
Endocones
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Beaded Calcified Siphuncle
Beaded Calcified Siphuncle
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Cameral Deposits
Cameral Deposits
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Ascocones
Ascocones
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Brevicone
Brevicone
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Coiling in Cephalopods
Coiling in Cephalopods
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Whorl Expansion Rate Formula
Whorl Expansion Rate Formula
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Aperture Distance Formula
Aperture Distance Formula
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Study Notes
Hierarchical Classification and Taphonomy
- Hierarchical classification: Domain, Kingdom, Phylum, Subphylum, Class, Order, Family
- Taphonomy defines changes between an organism's death and its discovery as a fossil
- Controls the fidelity of the fossil record and provides crucial environmental insights
- Paleoecology studies fossilized organisms, their life, and their environment
Fossils
- Fossil: any object that provides evidence of prehistoric life
- Types of fossils include physical remains, mineral replacements, biological impressions, and chemical signatures
Fossil Preservation
- Modes of fossil preservation vary from least to most information loss: unaltered soft parts, altered soft parts, unaltered hard parts, altered hard parts, leached fossils, biogenic structures, and biomarkers
Soft Part Preservation
- Unaltered soft parts show no change to organic tissues, except for water loss
- Preservation methods are restricted to recent Earth history and include freezing, mummification, and conservation traps
- Altered soft parts experience carbonization or mineralization of organic tissues, common since the Phanerozoic, often under anoxic conditions or rapid burial Fossil Lagerstätten ("motherlodes" of fossils) features excellent preservation of soft tissues and articulated hard parts
Hard Part Preservation
- Unaltered hard parts retain their original mineral composition
- Calcite (LMC) yields brachiopods, bryozoans, paleozoic corals, and echinoderms
- Aragonite yields molluscs and modern corals
- Silica yields radiolaria, diatoms, and some sponges
- Phosphate yields vertebrate bones, conodonts, and inarticulate brachiopods
- Chitin/collagen yields arthropods and graptolites
- Cellulose yields wood and plant material
Altered Hard Parts
- Recrystallization changes the crystal structure without altering the chemical composition, sometimes with water loss
- Aragonite (CaCo3) becomes LMC (CaCo3), and silica becomes quartz losing water
- Any mineral changes resulting from fine to coarse crystals
- Carbonization removes volatile elements through heat and pressure, leaving a carbon film, as seen in coal or graphite
- Permineralization (petrification) infills skeleton pores with minerals that precipitate from fluids, turning the material into stone
- Common with silicified wood and permineralized dinosaur bones
- Replacement occurs as the original skeleton dissolves, replaced by a new mineral such as dolomite, silica (opal), pyrite (under anoxic conditions), or limonite/goethite (iron hydroxides)
Leached Fossils
Original shell dissolves, leaving a void or filling with minerals, this is common in molluscs because aragonite dissolves easily
Fossil Molds
- Steinkern (core) shows internal features only, such as muscle attachments
- Cast features internal and external features
- Replica features only external features
- Mold features external features only, preserving shell structure
Sedimentary Structures Types
- Stromatolites are fossilized bacterial structures built by cyanobacteria in environments where grazers are absent and are abundant before grazing animals evolved
- Thrombolites are unlaminated, clotted microbial buildups
- Trace fossils are tracks, trails, burrows, and borings
- Coprolites are fossilized feces
Biomarkers
- Biomarkers are chemical evidence of life
- Hopanepolyol is an organic compound from bacterial cell walls
- Hopane is an organic compound derived from hopanepolyol
- Cholesterol can indicate the animal kingdom
Biostratinomy and Abrasion
- Biostratinomy covers events from an organism's death to its final burial, involving loss of biological information and gain of depositional insights
- Disarticulation involves the removal of joints and complete arthropods and echinoderms can only be preserved through obrution
- Abrasion is wear from transport measured usings Mohs Hardness Scales
Transport and Reorientation
- Transport via traction currents (bedload) causes extensive abrasion, while suspension causes minimal abrasion
- Storm beds and turbidities happen with currents/flows with higher density
- Reorientation aligns shells with currents/waves
- Unimodal orientation has all apices pointing in the same direction if current is flowing in one direction (direction isn't identifiable)
- Bimodal orientation has apices pointing in two directions (180° apart), indicating oscillating current
Shells
- Shells flip after a threshold, and concave-down orientation indicates wave or current activity, strong enough to flip the shells but too weak to orient them, or too strong and has strong bimodal orientation
- Dissolution is when shells dissolve in cold/freshwater, and can also occur prior to burial
Transportation Types
- Indigenous fossils are found in their original environment, but shuffled around, providing close information of what was living there
- Exotic fossils are transported from a different environment but (same time), and mix different communities
- Reworked (remanie) fossils are older fossils mixed with new sediments and can mislead age dating
Paleoecology
- Paleoecology helps understand ecosystem evolution, limiting factors, and explains responses to climate change and how complexity increases over time
- Limiting factors control species presence and abundance
Limiting Factors
Sedimentologic Factors
- Grain size influences organism types and abundance, with mobile sand supporting epifauna and less-mobile mud and gravel supporting easier organism attachment
- Substrate consistency affects benthic organisms, with sand being easiest for burrowing and gravel being hardest
- Turbulence hinders fragile/branching organisms
Metabolic Factors
- Light affects photosynthesis and vision, decreasing in quantity and wavelength spectrum with depth,
- Salinity affects diverse life, with freshwater and euryhaline environments leading to decrease in diversity and size
- Oxygen abundance affects predator rates and size
- Light zones influence life
Zone Classification
- Euphotic Zone Sunlight penetrates and allows photosynthesis to occur.
- Disphotic Zone Twilight zone where animals have eyes
- Aphotic Zone Midnight zone with no light and many blind animals
Depth/Ecological Factors
- Influence ecosystem with depth on following factors
- Grain Size
- Turbulence
- Light intensity
- Temperature
- Oxygen
- Body size
Trophic Classifications
- Individual Single organism
- Population Same spieces in one location or time
- *Community * All populations in one location or time
- Ecosystem Interaction of all organisms
Trophic Chain
- Energy and matter that flows from organism to orgamism
- Chemoautotrophs extract energy from organic material, begin with green plants and phytoplankton
Ecological
- Level organisms obtain energy and matter through the sam # of steps
- Autotrophs level 1
- Herbivores revel 2
- Carnivores level 3
- Omnivores fill all levels
Fauna Tiers
- Pelagic Lives in the water column
- Pleustonic Neustonic surface dwellers
- Planktonic Freely floating
- Nektonic Swimming
- Benthic Lives on the ocean floor
- Epifaunal Resides upon or extends into the water
- Infaunal Burrow/lives below the seal floor
Bambach cube
- Cube has 3 components
- Y axis; Organisms seal floor position
- X axis; Feeding strategy
- Z axis; Ability to move
Paleoecology
- *Marine *
- Similar limiting factors throughout
- More complete fossil record
- Increase over time
- Herbivory evolved faster
- Terrestrial* Longer time for life to move on land
- Uses smaller proxies Microfossils and isotopes Fossilize plant date
- Long to adapt Too longer to evolve
Trace fossils
- Preserved behaviours
- Foot print
- Not useful in biostratigraphy
- Very useful in paleoecology
Behavioural fossils
- Classified on behaviour
- Early, marine seawiigs
- Reinterpreted as tracks
- Trace fossils important for ancient enviornment
Organs of traces
- Behaviour
- Feeding traces
- Farming burrow
- Dwelling burrow
- Grazing traces
- Crawling traces
- Resting traces
- Escape burrower
- Walking / swimming traces
Environmental changes
- Increased depths increase pressure
- Decreased water energy with depth
- Low PH / limited sunlight
- Limited food and oxygen
General Ifaunas
- Names after ichnogenous of enviornment
- Main categories are
- Substrate controls
- Depth controls
Depth controls
- Hard to find, but include cemented surfaces, shelled, woody surfaces and materials
Ichno Facies
- Sandy shores dwelling animals
- Food in suspension
- No moment required
- Low burrow
- Sressful enviornment
Sublittoral
Food on the sea floor Shallow
Sealevels
- Record environmental transistions
- Sediment movement leads to environmental transistion
- Can combine Assemblages
Bivalves
- Pylum mullasca Most diverse animal pylym Wide ange of enviornmetns Best known invertebrates
Features
- 2 hinged halved
- Benthic animal
- Best fossils
- Reflects sediment consitency
Soft Parts
- Mantle produces and provides shell layers
- Psterior / anterior muscle controlled 2 shells
- Can excrete waste
- Dig with limbs
Single Symmetry
Can be found in the valves
Bibranch
- Suspension feed
- Small prey for feeeding
Shape
Exterior Body is attached to point Where mantel attach Interior
Bivalves
-
Are small and close
-
One or one large
-
One large
-
Can show symmetry
-
Long and wide teeth in subquel area
-
Little teeth for easy access
-
Small sockets to align valves and ligaments
-
Most common in mordern tropes
-
In bulnt teeth, or a reduced set
Bivalve growth
- Grows by adding material
- Can be used to read climate from material
Subgrounds
- protobranchia, filibranchia,eulamelibranchia,septibranchia Blended traits Mostly biological components Classified zoologically by traits biological
Bivalies
- Diversity Increased steadly through their range
- Outcompeted branchpods More mobile adaptable
Bivalve origin
- Origionated Jurassic
- Symbiotic algae
- Life style/ behaviour
Surifical Bysatte
Most modern live animals Some buried in sediment Berring shells bore into shells
Bivalve Burrow
- Can have small or long shlels
- Shell thinenes corelates with bourowing behavior
- How quaikly can
Cepal pods/ Ammunitions
- Similar in Bivalives in small group
- Exculivley marine
- Ammush style
- Tentacles grab prey
- Good vision
- eat softer pret better
Regulared buoyancy
- Allows adptation in the Water column
- No change to moulting
- Different from adults
Types
- Periostracum
- Prismatilc
- Nacreous outerlayer
Nautillis
- Where bodies emerge
- Help represent stages of morphology
Cephalopods
- chambers, bodies buoyancy, separate shell
Shelled
- Grotwh patterns in lines can assist species type and date the specimen
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