Taxonomy of commonly fossilised invertebrates

Source: Wikipedia, the free encyclopedia.
cystoid Echinosphaerites (an extinct echinoderm of the Class Rhombifera) from northeastern Estonia; encrusted by a graptolite
(black branches).

fossil record, ranging from protists to arthropods. The taxonomy discussed emphasizes invertebrates that are either frequently collected as fossils or are extinct. This includes groups that are significant in paleontological contexts, abundant in the fossil record, or have a high proportion of extinct species
. Special notations are explained below:

  • [ ! ]: Indicates clades that are important as fossils or very abundant in the fossil record.
  • [ – ]: Indicates clades that contain a large proportion of extinct species.
  • [ † ]: Indicates clades that are completely extinct.

The paleobiologic systematics that follow are not intended to be comprehensive, rather encompass invertebrates that (a) are popularly collected as fossils and/or (b) extinct. As a result, some groups of invertebrates are not listed.[1]

If an invertebrate animal is mentioned below using its common (vernacular) name, it is an extant (living) taxon, but if it is cited by its scientific genus, then it is typically an

fossil record.[2]

Invertebrate clades that are important fossils (e.g.

index fossils), and/or clades that are very abundant as fossils (e.g. crinoids, easily found in crinoidal limestone),[3]
are highlighted with a bracketed exclamation mark [ ! ].

Domain of
Eukaryota
/Eukarya

Quinqueloculina, a foraminiferan (a type of protist) from Donegal Bay, Ireland.

organized nucleus with DNA
.

Sub-domain of
Opisthokonta

fungi
; true animals.

  • most life forms documented, extinct or extant.
    • excludes: many molds; all one-celled protists (
      protoctists
      ); all algae; all green plants.

Kingdom of
Metazoa
- All Invertebrates and Vertebrates

).

  • comprises most living and deceased species which have ever been recorded, extinct or extant.
    • excludes all
      fungal
      opisthokonts.

Sub-kingdom of Parazoa

Parazoans; typically

marine invertebrates
.

Phylum
Archeocyathida
/Pleospongia [†]

Cone-shaped

archeocyathids; cup-shaped archaeocyathans/archeocyathans; reef-building pleosponges;calcareous
"ancient-cups".

Includes fossil

genera
such Archaeocyathus, Cambrocyathus, Atikonia, Tumuliolynthus, Kotuyicyathus, Metaldetes, Ajacicyathus and Paranacyathus.

Archaeocyatha is sometimes classified as a

Porifera
below.

Phylum

Pattersonia ulrichi Rauff, 1894; an Ordovician hexactinellid sponge from near Cincinnati, Ohio.
MUSE - Science Museum in Trento

Quintessential

siliceous – half of all documented species of Porifera are fossils and extinct.[4]

Porifera may eventually be broken up into separate phyla:

Sub-kingdom of Eumetazoa

Eumetazoans
; true metazoans (typically mobile, multicellular animals).

Eumetazoa contains most of the living and deceased species of recorded life, including most invertebrates (extinct and extant), as well as all vertebrate animals.

Super-phylum of Radiata

Radiates; non-bilaterian eumetazoans.

Phylum Cnidaria/Coelenterata

Aulopora (a tabulate coral) from the Silica Shale (Middle Devonian), northwestern Ohio.

coelenterates
:

Super-phylum of
Protostomia
# 1

molluscs
.

Phylum Bryozoa/Ectoprocta/Polyzoa

Heterotrypa, a trepostome bryozoan from the Corryville Formation (Upper Ordovician) in Covington, Kentucky.

Bryozoans – half of all documented species of Bryozoa are fossils and extinct.[5]

  • Class
    bryozoans
    ):
    • Order
      Cheilostomata
      [!] (living, rimmed-mouthed moss animals)
    • Order Cyclostomatida (uncontracted, round-mouthed bryozoans including fossil Stomatopora)
    • Order Cystoporata [†] (extinct, minor group of moss animals)
    • Order
      Trepostomata
      [†] [!] (changed-mouthed bryozoans such as extinct Constellaria and Monticulipora)
    • Order Cryptostomata [†] [!] (round hidden-mouthed bryozoans such as Archimedes, Fenestrellina and Rhombopora)
    • Order Ctenostomata [†] (uncommon, comb-mouthed bryozoans)
    • Order Phylactolaemata (living, fresh-water bryozoans)

Phylum
Brachiopoda

Rhynchotrema dentatum, a rhynchonellid brachiopod from the Cincinnatian (Upper Ordovician) of southeastern Indiana.

mollusks
below) – 99% of all documented species of Brachiopoda are now extinct.

Phylum
Annelida

Segmented worms such as earthworms and leeches
.

Phylum Mollusca

Peltoceras solidum ammonite from the Matmor Formation (Jurassic, Callovian) in the Matmor Formation, Makhtesh Gadol, Israel.
Vermetid gastropod Petaloconchus intortus attached to a branch of the coral Cladocora; Pliocene of Cyprus.

Molluscs or

above.

Super-phylum of
Protostomia
# 2

Phylum
Tardigrada

Panarthropodic

water bears
.

Phylum Onychophora

Panarthropodic

velvet worms
, including proto-arthropodic fossils of Arthropleura and Aysheaia.

Phylum
Arthropoda

Elrathia kingii (trilobite) from the Wheeler Shale (Middle Cambrian), Utah.

Arthropods;

jointed legged creatures with an exoskeleton
.

Super-phylum of
Deuterostomia
/ Enterocoelomata

Second-mouthed

deuterostomians, such as chordates and echinoderms
.

Phylum
Echinodermata

Middle Jurassic (Callovian) crinoid pluricolumnals (Apiocrinites) from the Matmor Formation in Hamakhtesh Hagadol, southern Israel.

Echinoderms – 72% of all documented species of Echinodermata are fossils and extinct.[7]

Phylum
Hemichordata

Pendeograptus fruticosus graptolites from the Bendigonian Australian Stage (Lower Ordovician) near Bendigo, Victoria, Australia. Two overlapping, three-stiped rhabdosomes.

Hemichordates such as extant acorn worms – Less than half of the documented species of Hemichordata are fossils and extinct.

Phylum
Chordata

Both invertebrate and vertebrate chordates; animals possessing a notochord.

Invertebrate subphyla

  • Subphylum
    sea squirts
    )
  • Subphylum
    Cephalochordata (invertebrate lancelets
    )

Subphylum
Vertebrata

Deinosuchus hatcheri at the Natural History Museum of Utah.

See also

References

  1. ).
  2. zoologists
    Michael Hutchin, Dennis A. Thorney and Sean F. Craig (2003).
  3. ^ For correspondingly ancient ecosystems, see the Treatise on Ecology and Paleoecology, Volume 2: Paleoecology, edited for years by Harry S. Ladd (1957 / 1971), and published by both the Geological Society of America (Boulder, Colorado) and the Waverly Press (Washington, D.C.).
  4. ^ The rates of extinction for sponges and other phyla are derived from W. H. Easton, 1960, Invertebrate Paleontology (New York: Harper and Brothers) and various modern sources.
  5. ^ For bryozoans and brachiopods, the same footnote as above.
  6. ^ For bivalves and cephalopods (both mollusks), see the above notation.
  7. ^ For the echinoderms, see the above footnote regarding W. E. Easton, 1960, Invertebrate Paleontology, and other sources.