• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/86

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

86 Cards in this Set

  • Front
  • Back

Classification


Phylum Porifera


Class Archaeocyatha




About


Cambrian(abundant in early Cambrian)


Inner and outer walls form a ring, divided by septa


Base of the sponge attached to a hard substrate with a holdfast


Were first multicellular organisms to build reegs

Classification


Phylum Porifera


Class Hexactinellida




About


Cambrian to Recent


Called "glass sponges"


Colorless and have a plaid pattern

Classification


Phylum Porifera


Class Calcarea




About


Cambrian to recent


only found in marine


only have calcite spicules


can resemble Demospongia, but can be differentiated by effervescing with acid

Classification


Phylum Porifera


Class Demospongia




About


Pre-Cambrian to recent


most diverse sponge(~80%of all sponge species today)


Made of spogin &/or silica spicules


Doesn't fossilize well, so isn't very common in fossil record

Classification


Phylum Porifera


Class Stromatopoids




About


Cambrian to Neogene


Calcareous


Resemble stromatolites, but have vertical pillars between laminae


imporant reef builders in Devonian

Classification


Genus Receptaculitids




About


Ordovician to Devonian


The zoological affinities for receptaculids are currently uncertain. Recepeptaculitids is a genus name.


Some consider them sponges, but more are considering them calcareous algae


Their skeletons range from globular to discoidal forms


were probably attached to substrate by a fleshy stalk

Classification


Phylum Cnidaria


Class Anthozoa


Subclass Zoantharia


Order Scleractinia




About


Mid-Triassic to recent


Reef Builder


Scelartinia coral have a radial septa pattern during growth


Their septa usually grow in multiples of 6


Their septa are exsert and extend above the rim of the corallite


These septa make ridges called costae, along the epitheca as they grow


Classification


Phylum Cnidaria


Class Anthozoa


Subclass Zoantharia


Order Rugosa




About


Ordovician to Permian




Can be solitary or cononial




Septa grew in distinct quadrants




They exclusively lived in warm water




Not reef builders




Several different colonial growth forms









Scleractinia vs. Rugosa




Rugose corals do not have exsert septa or costae like Scleractinian corals


Rugosa septa grew in quadrants, while Scleractinian septa grows in multiples of 6.

Classification


Phylum Cnidaria


Class Anthozoa


Subclass Zoantharia


Order Tabulata


Suborder Favositina




About


Mid-Ordovician to Permian


Ceroid corallum(Polygonal to subcircular corralites)


Individual corallites connected via mural pores in the walls of corallite

Classification


Phylum Cnidaria


Class Anthozoa


Subclass Zoantharia


Order Tabulata


Suborder Aulaporina




About


Mid-Ordovician to Permian


Each Corallite is a distinct tube in a branching corallum


Reptant growth form



Classification


Phylum Cnidaria


Class Anthozoa


Subclass Zoantharia


Order Tabulata


Suborder Halysitina




About


Mid-Ordovicain to Late Silurian


Corallites are elliptical cylinders and join in chains with no mural pores


Cateniform growth form

Classification


Phylum Cnidaria


Class Anthonzoa


Subclass Zoantharia


Order Tabulata


Suborder Syringoporina




About


Mid-Ordovician to Permian


Fasciculate corallum with roughly cylindrical corallites joined together by tubes


Occur in warm, shallow warms but not reef builders

Classification


Phylum Mollusca


Class Polyplacophora




About


Cambrian to recent


Marine animals


Commonly called chitons


Live in rocky intertidal areas


They have 8 calcareous plates on top of the girdle (Girdle is thick mantle tissue covered by a thing cuticle, sometimes embedded with calcite spicules)


Graze on algae using their radula

Class Gastropoda

Cambrian to recent


Environmentally widespread


range of feeding habits


Their foot drags them along or lets them burrow


Many have an inhalant siphon they use to take in water( it extends through the siphonal canal)

Classification


Phylum Mollusca


Class Gastropod


Caenogastropods




About


Cambrian to recent


Have an inhalant siphon that is usually apparent by a siphonal canal





Classification


Phylum Mollusca


Class Gastropod


Archaeogastropods




About


Cambrian to recent


Lack an inhalant siphon and a siphonal canal, but compensate by having holes or slits in the shell for exhalent current


Their slit can create a band on the growth lines of the shell called a selenizone



Limpets




Archaeogastropods

Class Bivalvia

Cambrian to recent




marine and freshwater




different epifaunal and infaunal lifestyles


filter feeds




made up of a left & right calcareous valve




Bilaterally symmetrical between the valves



Classification


Phylum Mollusca


Class Bivalvia


Burrower




About


use their foot and open & close their shell to dig deeper into sediment


Enlarged pallial sinur and adductor muscles


Potentially gaped shell for larger siphon

Classification


Phylum Mollusca


Class Bivalvia


Byssally attached




About


attach to hard surfaces by organic threads(byssal threads), like mussels


Reduced foot and Pallial sinus


Better developed teeth and thicker shell for defense



Classification


Phylum Mollusca


Class Bivalvia


Rudists




About


Conical right valve with a small lid-like left valve


Asymmetrical, Reef builders





Classification


Phylum Mollusca


Class Bivalvia


Borer




About


bore into rock, wood, or shells either mechanically or by secreting acid chemical that dissolves calcium carbonate

Classification


Phylum Mollusca


Class Bivalvia


Cementers




About


Secrete hard bonding agent to attach to surfaces or other organisms, like oysters


Asymmetrical


Scar on the shell where they attached



Classification


Phylum Mollusca


Class Bivalvia


Epifaunal free-lying




About


Sit on the sediment with no attachment


Asymmetrical, thick, heavily curved bottom valve, with much smaller top valve


Single adductor muscle. and reduced to no teeth


"Devils Toe"

Classification


Phylum Mollusca


Class Bivalvia


Swimmers




About


Scallops are a type of epifaunal free-lying bivalve with the ability to quickly shut both valves to squirt out water to propel themselves in short bursts


symmetrical through the valves(like Brachs)



Class Cephalopda

Coiled Shells


-Evolute: each coil is visible


-Involute: Only the last coil is visible, the rest are tucked within the shell. Some groups are partly involute




Cone Shells


-Orthoconic: Completely straight cone


-Cyrtoconic: Curved Cone

Classification


Phylum Mollusca


Class Cephalopoda


Subclass Naulitoidea


Order Endoceratida




About


Ordovician to Silurian


Orthocone or cyrtoocone with large siphuncle


Has endosiphuncular deposits


In cross-section, deposits make a "cone-in-cone" structure, called endocones

Classification


Phylum Mollusca


Class Cephalopoda


Subclass Naulitoidea


Order Actinoceratida




About


Ordovician to Carboniferous


Usually orthoconic shells


Siphuncle expands between septa, creating bulbous endosiphuncular


Can also have cameral deposits



Classification


Phylum Mollusca


Class Cephalopoda


Subclass Nautiloidea


Order Nautilida




About


Devonian to recent


Complete to partly involute shells


Suture lines are straight, curved, or gently sinous


Suture lines are only visible on Internal Molds

Subclass Ammonoidea

Coiled shells

More complex suture lines than Nautiloids

Siphuncle runs along the edge of the shell

Coiled shells




More complex suture lines than Nautiloids




Siphuncle runs along the edge of the shell



Classification


Phylum Mollusca


Class Cephalopoda


Subclass Ammonoidea


Order Goniatitida




About


Devonian to Permian


Goniatitic sutures( Pointed lobes, rounded saddles)


Involute Shells

Classification


Phylum Mollusca


Class Cephalopoda


Subclass Ammonoidea


Order Ceratitida




About


Triassic


Ceriatitic sutures (smooth saddles, folded lobes)


Involute or evolute shells

Classification


Phylum Mollusca


Class Cephalopoda


Subclass Ammonoidea


Order Ammonitida




About


Jurassic to Creaceous


Ammonitic Sutures (complex and flame-like)


Involute or evolute shells

Classification


Phylum Mollusca


Class Cephalopoda


Subclass Ammonoidea


Order Ammonitida


Suborder Lytoceratina




About


Jurassic to Creaceous


Group called "heteromorphs" is mainly Creaceous


Ammonitic sutures


Partly uncoiled, some parts appear straight (especially when fragmented)


Thought to be passive floaters, rather than swimmers, that fed on plankton

Classification


Phylum Mollusca


Class Cephalopoda


Subclass Coleoidea


Order Belemnitida




About


Late Carboniferous to Cretaceous


Shell (pro-ostracum, phragmocone, siphuncle, and guard) is entirely internal, covered by the mantle


The guard is bullet-shaped and has a radial fibrous crystal growth


The phragmocone fits into a cone-shaped depression in the end of the guard



Classification


Phylum Mollusca


Class Scaphopoda




About


Ordovician to recent


"Tusk Shells"


Tapered, cylindrical shell


The animal lives in the sediment with larger opening down and the top of the shell above the sediment to take in water


They are deposit feeders and carnivores. using tentacles to capture prey

Classification


Phylum Brachiopoda


Subphylum Rhynchonelliformea


Order Orthida




About


Cambrian-Permian


Both valves convex, typically with more convex of the ventral value


Hinge is typically wide with well developed interarea and open delthyrium



Classification


Phylum Brachipoda


SubphylumRhynchonelliformea


Order Strophomenida


Suborder Strophomenidina




About


Ordovician-triassic


Shell broad and slender, with gently convex ventral valve and flat to concave dorsal valve


Have "snow-shoe" adaptions for dealing with soft, relatively fluid, muddy bottoms

Classification


Phylum Brachiopoda


SubphylumRhynchonelliformea


Order Strophomendia


Suborder Chonetidina




About


Silurian-Jurassic


Shells are slender, with convex ventral and flat to concave dorsal valves.


Row of delicate spines arasing from the ventral value interarea (often broken off with only bases visible)

Classification


Phylum Brachiopoda


Subphylum Rhynchonelliformea


Order Strophomendia


Suborder Productidina




About


Devonian-Permian


Ventral Valve strongly convex and carries tubular spines on surface (often broken off with only bases visible)


Dorsal valve concave

Classification


Phylum Brachipoda


Subphylum Rhynchonelliformea


Order Spiriferida




About


Silurian-jurassic


Wide, biconvex shells with laterally directed, spirally-coiled brachidium


Ventral valve commonly much taller than dorsal valve with well-developed interea

Classification


Phylum Brachiopoda


Subphylum Linguliformea


Order Lingulida




About


Cambrian-Recent


Valves are roughly elliptical in outline and similar in size


Pedicle emerges between the edges of the valves





Classification


Phylum Brachipoda


Subphylum Linguliformea


Order Acrotretida




About


Cambrian-recent


Nearly flat, circular dorsal valve and a conical ventral valve


Pedicle, when present, emerges through an opening in the ventral valve

Classification


Phylum Brachiopoda


Subphylum Rhynchonelliformea


Order Terebratulida




About


Devonian-recent


Diconvex shells


Fairly smooth exterior


Usually large beak with well-developed foramen


Brachidium is a simple or complex loop





Classification


phylum Brachiopoda


Subphylum Rhynchonelliformea


Order Rhynchonellida




About


Ordovician-recent


Usually biconvex shells


Well-developed ribs on exterior


Small beak and small formaen

Classification


Phylum Brachipoda


Subphylum Rhynchonelliformea


Order Pentamerida




About


Mid-Cambrian-Devonian


Biconvex shells


Lacks a pedicle opening


Ventral valves has a distinct muscle attachment structure called a spondylium( Y-shaped in cross-section, and dorsal valve can have a corresponding structure called the cruralum



Classification


Phylum Brachipoda


Subphylum Rhynchonelliformea


Orde Atrypida




About


Ordovician-Devonian


Has a spiral brachidium (spiralia) that is oriented vertically


Dorsal Valve is much more convex than the ventral valve (dorsal valve is inflated to accommodate the spiralia)



Classification


Phylum Arthropoda


Subphylum Chelicerata


Class Merastomata


Subclass Xiphosura




About


Cambrian?:Silurian to recent


Horseshoe crabs


Two tagmata (the prosoma and opisthosoma, the adbomen & telson)



Classification


Phylum Arthropoda


Subphylum Chelicerata


Class Merastomata


Subclass Eurypterida




About


Ordovician-Permian


Short Prosoma


Long, narrow opisthosoma


5 pairs of legs

Classification


Phylum Arthropoda


Subphylum Crustacea


Class Malacostraca




About


Cambrian-recent


Accounts for over half of living crustaceans


3 tagmata(5 segmented head, 8 segmented thorax, 6 segmented abdomen+telson)



Classification


Phylum Arthropoda


Subphylum Crustacea


Class Cirripedia




About


?Cambrian-rect


Barnacles are attached epifuanal suspension feeders


Body enclosed by a carapace with overlapping calcareous plates, called lateral plates


Two pairs of plates form the operculum, which open to allow the appendages to extend


Six Pairs of appendages called cirri used for feeding

Classification


Phylum Arthropoda


Subphylum Crustacea


Class Ostracoda




About


Cambrian-recent


small, aquatic crustaceans


greatly modified body enclosed in a carapace made of two halves


well-developed head appendages, rest of body is reduced

Classification


Phylum Arthropoda


Subphylum hexapoda




About


Devonian to recent


Insects


Very diverse


3 tagmata


Uniramous appendages

Classification


Phylum Arthropoda


Agnostoid arthropods




About


Cambrian-Ordovician


small trilobite-like arthropods


3 tagmata(cephalon, thorax, pygidium)


Calcite exoskeleton


No eyes, 2 thoracic segments


limbs differ from those of trilobites



Class Trilobita

Cambrian to Permian


Marine Arthropods that lived on the seafloor(shallow and deep waters)


Preyed on small inverts, ate algae, &/or were scavengers


Reproduced sexually, may have had brood pouches

Classification


Phylum Arthropoda


Class trilobita


Order Eodiscida




About


cambrian


Resemble agnostoid


small, isopygous


Marginal sutures


2-3 thoracic segments


Pygidial axis is well segmented; has numerous axial rings



Classification


Phylum Arthropoda


Class Trilobita


Order Redlichiida


Suborder Olenellina




About


Lower Cambrian


Micropygous


Thoracic segments extend into spines


Marginal sutures


Large, crescent-shaped, holochroal eyes, close to glabela


Lacked a calcified protaspis stage



Classification


Phylum Arthropoda


Class Trilobita


Order Redlichiida


Suborder Redlichiina




About


Lower to Middle Cambrian


Differs from Olenellina by having Opisthoparian facial sutures


Calcified protaspis stage present

Classification


Phylum Arthropoda


Class Trilobita


Order Ptchopariida




About


Cambrian-Ordovian


"Garbage can" taxa group


Micropygous


Ospithoparian sutures


Small, holochroal eyes


Numerous thoracic sements


usually 2-3 pairs of glabellar furrows

Classification


Phylum Arthropoda


Class Trilobita


Order Corynexochida


Suborder Corynexochina




About


Cambrian


Isopygous(usually)


7-9 thoracic segments


Pygidium has well-developed segmentation


Glabella is parallel-sided and extends forwards

Classification


Phylum Arthropoda


Class Trilobita


Order Corynexochida


Suborder Illaenina




About


Ordovician-Devonian


Isopygous


Opisthoparian sutures


Can be extremely smooth, or have a foward expanding glabella with large tail with a short axis and well-developed interplueral furrows

Classification


Phylum Arthropda


Class trilobita


Order Asaphida


Suborder Asaphina




About


Upper Cambrian to Ordovician


Smooth, Isopygous, opisthoparians


Usually 8 thoracic segments


Sutures converge to a point on the anterior border


Largest know trilobite is an asaphina

Classification


Phylum Arthropoda


Class Trilobita


Order Asaphida


Suborder Trinucleina




About


Upper Cambrian-Lower Silurian


Isopygous


Marginal or opisthoparain sutues


Unique cephalon, with a pitted fringe, teardrop-shaped glabella, long genal spines (often break off during taphonomy)


5-7 thoracic segments


Triangular-shaped Pygidium

classification


Phylum Arthropoda


Class trilobita


Order Harpida




About


upper cambrian-Devonian


Micropygous


marginal sutures


At least 12 thoracic segments


Small eyes, or blind


Large Cephalon with long, broad genal spines, sometimes pitted. Glabella norrows forwardly

Classification


Phylum Arthropoda


Class Trilobita


Order Proetida




About


Ordovician to Permain


Micro-or isopygous


Opisthoparian


Eyes are close to glabella


Glabellar furrows are curved


Pygidium usually large with several axial rings

Classification


Phylum Arthropoda


Class Trilobita


Order Phacopida


Suborder Phacopina




About


Ordovician-Devonian


Proparian Sutures


Isopygous


Schizochroal eye (only group that has them)


Large glabella that expands forwards


Normally 11 thoracic segments

Classification


Phylum Arthropoda


Class trilobita


Order Phacopida


Suborder Cheirurina




About


Ordovician-Silurian


Micropygous


Proparian


Holochroal eyes


Rectangular glabella with deep furrows (some have a "bow tie")


Spines on pygidium

Classification


Phylum Arthropida


Class trilobita


Order Phacopida


Suboorder Calymenina




About


Ordovician-Devonian


Gonatoparian


Very small eyes


13 thoracic segments


Glabella is forwardly tapered with deep furrows OR is rectangular in shape with weak furrows

Classification


Phylum Arthropida


Class Trilobita


Order Odontopleurida




About


Ordovician-Devonian


Iso- or Miscropygous


Opisthoparian


Highly spinose


Quadrate (meaning 4) furrowed glabella


Sometimes has a "toothed" border along free checks

Classification


Phylum Arthropida


Class Trilobita


Order Lichida




About


Late Cambrian-Devonian


Opisthoparian


Glabellar lobes are inflated and fused


Pygidium often has 3 pairs of leaf-like or spinose pleural structures


Often covered in tubercles



Classification


Phylum Bryozoa


Dome-Shaped Bryozoa





Classification


Phylum Bryozoa


Branching bryozoa



Classification


Phylum Bryozoa


Fan-shaped Bryozoa



Classification


Phylum Hemichordata


Class Graptolithina


Order Dendroidea




About


Mid-Cambrian to Carboniferous


Numerous stipes with hundreds of thecae, often connected by a rod-like structure


Rhabdosomes are conical, fan-like, or shrub like


Most were benthic & attached to sea floor, some were plankton



Classification


Phylum Hemichordata


Class Graptolithina


Order Graptoloidea


Suborder Didymongraptina




About


Ordovician


2-4 pendent to reclined stipes with simple theca



Classification


Phylum Hemichordata


Class Graptolithina


Order Graptoloidea


Suborder Diplograptina




About


Ordovician-Silurian


Two scandant stipes that grew back-to-back, enclosing the nema

Classification


Phylum Hemichordata


Class Graptolithina


Order Graptoloidea


Suborder Monograptina




About


silurian-lower Devonina


1 scandant stipe


Theca may possess an ornate, curved, or spinose aperture


A secondary stipe can form off a theca (called a cladia)

Classification


Phylum Echinodermata


Subphylum Asterozoa


Class Asteroidea




About


Ordovician-recent


Starfish


Predators & herbivors


Commonly has 5 arms, can be more (arms join at a central disc


Can usually see the Madreporite where the water enters

Classification


Phylum Echinodermata


Subphylum Asterozoa


Class Ophiuroidea




About


Ordovician-recent


Brittle stars


thing arms well-differentiated from central disc


Suspension feeders, deposit feeders, scavengers

Classification


Phylum Echinodermata


Subphylum Echinozoa


Class Echinoidea


Regular echinoid




About


Ordovician-recent


Sea urchins


Epifaunal


Mouth and a complex jaw apparatus called Aristotle's Lantern is located in the Peristome (Oral Surface)


Anus is located in the Periproct (Aboral Surface)


5 Ambulacral areas, 5 Interambulacral areas

Classification


Phylum Echinodermata


Subphylum Echinozoa


Class Echinoidea


Irregular Echinoids




About


Jurassic-recent


Heart urchins, sand dollars, sea biscuits


Periproct & anus is shifted, due to its infaunal habits


Spines are small & slender, except on oral surface which is longer & robust, used for locomotion


Petaloid Ambulacrum & Tube feet are well-defined on aboral surface

Classification


Phylum Echinodermata


Subphylum Crinozoa


Class Crinoidea




About


Cambrian-recent


stalked pelmatozoans


suspension feeders


3 skeletal areas: the cup-shaped calyx (body), arms (feeding structures), stem & Holdfast.

Classification


Phylum Echinodermata


Subphylum Blastozoa


Class Blastoidea




About


Silurian-Permian


Similar to Crinoids


Cup-shaped body (theca), a stem, and hold fast


Short arm structures called brachioles


Well-developed pentaradial symmetry and ambulacra


Holes at the top of the Theca (1 is the mouth, 1 is the Anus)

Classification


Phylum Echinodermata


Subphylum Blastozoa


Class Cystoidea




About


Ordovician-Devonian


Brachioles at the top of the golubar the test


Test lac pentaradial symmetry & the large ambulacral areas that blastoids have


Respirator openings at the plate boundaries (paired pores (diplopores) and Rhombic Regions of pores (pectinirhombs)

Classification


Phylum Echinodermata


Class Edrioasteroidea




About


Cambrian-Carboniferus


Immobile, epifaunal


Aboral surface permanently attached to hard surface


Mouth & Anus on oral surface, both covered by plates


Openings for tube feet on ambulacral area


Probably suspension feeders