Malone Formation

Last updated
Malone Formation
Stratigraphic range:
Kimmeridgian-Tithonian
~153–149  Ma
O
S
D
C
P
T
J
K
Pg
N
[1]
Type Geological formation
Sub-units
  • Upper member
  • Lower member
Underlies Torcer Formation
Overlies Briggs Formation [2]
Thickness
  • 45 meters (east side)
  • 325 meters (northwest part of Malone Mountains)
Lithology
PrimarySiliclastic strata & limestone [1]
Location
RegionFlag of Texas.svg  Texas
CountryFlag of the United States.svg  United States
Type section
Named forMalone Mountains

The Malone Formation is a geologic formation in Texas. It preserves fossils dating back to the Jurassic period.

Contents

Description

One of the few geological formations in Texas dating to the Jurassic period, the Malone Formation unconformably overlies the Permian Briggs Formation, [2] and laterally changes thickness dramatically from 45 meters on the east side to 325 meters in the northwest part of the Malone Mountains. [1] It has been split into two subdivisions: a lower member containing Idoceras suggesting a Kimmeridgian age, and an upper member containing Kossmatia indicating a Tithonian age. [2] Geochronological analysis of detrital zircon suggests an age of 151±2 Ma for the formation, supporting its dating to the late Jurassic. [1]

Depositional environment

The Malone Formation represents a fan-delta system in a shallow marine to marginal marine environment, deposited along the northern edge of the Chihuahua trough (a sedimentary basin mostly located in northeast Mexico). [1] Many fossils found in the formation represent marine invertebrates. [3]

Fossil content

Color key
Taxon Reclassified taxonTaxon falsely reported as presentDubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Vertebrates

Remains of vertebrates in this formation are rare and mostly poorly-preserved. Two cycloid fish scales, a pycnodont tooth and bone fragments of 'enaliosaurs' (a classification now obsolete) have been reported from the Malone Formation, but are not well-described. [3]

Vertebrates reported from the Malone Formation
GenusSpeciesPresenceMaterialNotesImages
cf. Plesiosauria Northwest Malone Mountains (Jackson Ranch area). [1] Propodial (TMM 47259–1). [1] A small, possibly juvenile plesiosaur.
cf. Pliosauridae Northwest Malone Mountains (Jackson Ranch area). [1] Vertebra (TMM 44038–1). [1] A pliosaur.

Invertebrates

Annelids

Annelids reported from the Malone Formation
GenusSpeciesPresenceMaterialNotesImages
Serpula S. gordialis1.5 miles east of Malone station. [3] Numerous specimens. [3] A tube worm.
S. sp.1.5 miles east of Malone station. [3] Multiple specimens. [3] Larger than S. gordialis.
S. sp.1.5 miles east of Malone station. [3] 1 specimen now lost. [3] Distinct from the other Serpula of the formation.

Bivalves

Bivalves reported from the Malone Formation
GenusSpeciesPresenceMaterialNotesImages
Anatina A. obliquiplicata1.5 miles east of Malone station. [3] 8 specimens. [3] A duck clam.
A.? pliculifera1.5 miles east of Malone station. [3] 1 specimen. [3] A duck clam.
Arca A.? dumbli1.5 miles east of Malone station. [3] 5 specimens. [3] An ark clam.
A. taffii1.5 miles east of Malone station. [3] 1 specimen. [3] An ark clam.
Astarte A. breviacola1.5 miles east of Malone station. [3] Numerous specimens. [3] An astartid.
A.? craticula1.5 miles east of Malone station. [3] 1 specimen. [3] An astartid.
A.? isodontoides1.5 miles east of Malone station. [3] 1 specimen. [3] An astartid.
A. malonensisVarious localities in & around Malone Mountain. [3] Numerous specimens. [3] An astartid.
A. posticalva1.5 miles east of Malone station. [3] 21 specimens. [3] An astartid.
Corbula C.? malonianaWest base of Malone Mountain. [3] Cast of a right valve. [3] A corbulid.
Cucullaea C. castilloiNorthwest end of Malone Mountain. [3] 2 specimens. [3] A false ark shell.
C. catorcensisEast of Malone Mountain. [3] 4 casts. [3] A false ark shell.
C.? texticostata1.5 miles east of Malone station. [3] 1 specimen & a fragment. [3] A false ark shell.
C. transpecosensis1 mile northeast of Malone, El Paso County, Texas. [3] 1 specimen. [3] A false ark shell.
Craginella C. goodellii2.4 km east for Malone station. [4] 18 specimens. [3] A megatrigoniid, originally reported as Trigonia goodelli. [4]
Cyprina C. coteroi1.5 miles east of Malone station. [3] 4 (& 2 doubtful) specimens. [3]
C.? streeruvitzii1.5 miles east of Malone station. [3] 11 incomplete specimens. [3]
Exogyra E. potosinaWest of Malone Mountain. [3] 6 specimens. [3] A gryphaeid.
E. subplicifera1.5 miles east of Malone station. [3] 19 specimens. [3] A gryphaeid.
Gervillia G. cinderellaWest base of Malone Mountain. [3] 1 specimen. [3] A bakevelliid.
G. corrugata1.5 miles east of Malone station. [3] 23 imperfect specimens & fragments. [3] A bakevelliid.
G.? riograndensisWest base of Malone Mountain. [3] 1 specimen. [3] A bakevelliid.
Gryphaea G. mexicanaVarious localities in & around Malone Mountain. [3] Numerous specimens. [3] A gryphaeid.
Leda L.? naviculaEast slope of Malone Mountain. [3] Cast of a left valve. [3]
Lima L. interlineata1.5 miles east of Malone station. [3] Valves & fragments. [3] A file shell.
L. (Ctenostreon) riograndensis1.5 miles east of Malone station. [3] 1 specimen. [3] A file shell.
Lucina L.? emarginata1.5 miles east of Malone station. [3] 3 specimens. [3] A lucinid.
L. planiusculaNorthwest end of Malone Mountain. [3] 4 shells & about a dozen casts. [3] A lucinid.
L. potosina1.5 miles east of Malone station. [3] 5 specimens. [3] A lucinid.
L. potosina var. metricaVarious localities in & around Malone Mountain. [3] Over 200 specimens. [3] A lucinid.
Martesia M. malonianaVarious localities in & around Malone Mountain. [3] Casts. [3] A piddock.
Modiola M. geniculata1 mile east of Finlay station. [3] A left valve. [3] A mussel.
M. malonianaVarious localities in & around Malone Mountain. [3] 4 specimens. [3] A mussel.
Mytilus M. nuntius1.5 miles east of Malone station. [3] A well-preserved cast. [3] A mussel.
Ostrea O. sp.1.5 miles east of Malone station. [3] 3 imperfect valves. [3] A true oyster.
Pecten P. (Camptonectes) insutusVarious localities in & around Malone Mountain. [3] About 50 specimens. [3] A scallop.
Pholadomya P. marcoui1.5 miles east of Malone station. [3] 10 specimens. [3] A pholadomyid.
P. paucicosta1.5 miles east of Malone station, & 2 miles east-southeast from Finlay station. [3] 27 specimens. [3] A pholadomyid.
P. praeposita1.5 miles east of Malone station. [3] 4 specimens. [3] A pholadomyid.
P. tosta1.5 miles east of Malone station. [3] 25 specimens. [3] A pholadomyid.
Pinna P. quadrifronsVarious localities in & around Malone Mountain. [3] Numerous specimens. [3] A pen shell.
Pleuromya P. inconstansVarious localities in & around Malone Mountain. [3] Numerous specimens. [3]
P. inconstans var. curtaSouthern part of Malone Mountain & 1.5 miles east of Malone station. [3] Multiple specimens. [3]
Plicatula P. sportella1.5 miles east of Malone station. [3] 1 specimen. [3] A plicatulid.
Ptychomya P. stantoni1.5 miles east of Malone station. [3] 23 specimens. [3] A crassatellid.
Tapes T.? cuneovatus1.5 miles east of Malone station. [3] A right valve. [3] A venus clam.
Thracia T.? maloniana1.5 miles east of Malone station. [3] 6 specimens. [3] A thraciid.
Trigonia T. calderoni1.5 miles east of Malone station, & a mile east of Finlay station. [3] 11 specimens. [3] A trigoniid.
T. conferticostata1.5 miles east of Malone station. [3] A shell, 2 valves & fragments. [3] A trigoniid.
T. goodellii1.5 miles east of Malone station. [3] 18 specimens. [3] Reassigned to Craginella .
T. munitaWest & east of Malone station. [3] 3 imperfect specimens & several fragments. [3] A trigoniid.
T. praestriataEast slope of Malone Mountain. [3] A mold. [3] A trigoniid.
T. proscabra1.5 miles east of Malone station. [3] About 35 specimens. [3] A trigoniid.
T. rudicostata1.5 miles east of Malone station. [3] 2 specimens. [3] A trigoniid.
T. vyschetzkii1.5 miles east of Malone station. [3] Numerous specimens. [3] A trigoniid.
Unicardium U.? semirotundumVarious localities in & around Malone Mountain. [3] 12 specimens. [3] A lucinid.
U.? transversumVarious localities in & around Malone Mountain. [3] 16 specimens. [3] A lucinid.

Bryozoans

Bryozoans reported from the Malone Formation
GenusSpeciesPresenceMaterialNotesImages
Berenicea B. maloniana1.5 miles east of Malone station. [3] Colonies. [3] A bereniceid.

Cephalopods

Cephalopods reported from the Malone Formation
GenusSpeciesPresenceMaterialNotesImages
Aspidoceras A. alamitocensis1.5 miles east of Malone station. [3] Portion of a shell. [3] An ammonite.
Nautilus N. burkartiWest side of the mountain southwest of Malone station. [3] An imperfect specimen. [3] A nautiloid.
N. naufragusNorthwest end of Malone Mountain. [3] 2 imperfect specimens. [3] A nautiloid.
Olcostephanus O. malonianus1.5 miles east of Malone station. [3] A few parts of the whorls. [3] An ammonite.
Oppelia O.? fallax1.5 miles east of Malone station. [3] Fragmentary specimens. [3] An ammonite.
Perisphinctes P. aguileraiFoothills west of Malone Mountain. [3] 7 fragments. [3] An ammonite.
P. clarkiVarious localities in & around Malone Mountain. [3] Multiple specimens. [3] An ammonite.
P. felixi1.5 miles east of Malone station. [3] 2 specimens. [3] An ammonite.
P. potosinus1.5 miles east of Malone station. [3] Fragment. [3] An ammonite.
P. schuchertiVarious localities in & around Malone Mountain. [3] Multiple specimens. [3] An ammonite.

Corals

Corals reported from the Malone Formation
GenusSpeciesPresenceMaterialNotesImages
Astrocoenia A. maloniana1.5 miles east of Malone, Texas. [3] 9 specimens. [3] An astrocoeniid.

Echinoderms

Echinoderms reported from the Malone Formation
GenusSpeciesPresenceMaterialNotesImages
Holectypus H.? sp.East slope of Malone Mountain. [3] A fragment. [3] A sea urchin.
Pygurus P. sp.West side of Malone Mountain. [3] A fragment. [3] A sea urchin.

Gastropods

Gastropods reported from the Malone Formation
GenusSpeciesPresenceMaterialNotesImages
Acteonina A.? maloniana1.5 miles east of Malone station. [3] Cast bearing 2 fragments. [3] An acteonid.
Cerithium C. arcuiferum1.5 miles east of Malone station. [3] 1 specimen. [3] A cerith.
Delphinula D. stantoni1.5 miles east of Malone station. [3] 5 specimens. [3]
Natica N. bilabiata1.5 miles east of Malone station. [3] 1 specimen. [3] A moon snail.
N. finlayensisNorthwest end of Malone Mountain. [3] 1 specimen. [3] A moon snail.
N. inflecta1.5 miles east of Malone station. [3] 3 shells. [3] A moon snail.
N. williamsi1.5 miles east of Malone station. [3] Nearly 100 specimens. [3] A moon snail.
Nerinea N. circumvoluta1.5 miles east of Malone station. [3] Several specimens. [3] A nerineid.
N. goodellii1.5 miles east of Malone station, & southern end of Malone Mountain. [3] Multiple specimens. [3] A nerineid.
Nerinella N. stantoniVarious localities in & around Malone Mountain. [3] Several specimens. [3] A nerinellid.
Nerita N. finlayensisNorthwest end of Malone Mountain. [3] 1 specimen. [3] A nerite.
N. nodilirataLower strata. [3] 54 specimens. [3] A nerite.
N. peroblata1.5 miles east of Malone station. [3] 1 specimen. [3] A nerite.
Pleurotomaria P. circumtrunca1.5 miles east of Malone station. [3] 11 specimens. [3] A pleurotomariid.
Pseudomelania P. goodelliiVarious localities in & around Malone Mountain. [3] Multiple specimens. [3] A pseudomelaniid.
Turbo T.? beneclathratus1.5 miles east of Malone station. [3] 1 specimen. [3] A turban snail.
Turritella T. burkartiEast slope of Malone Mountain. [3] 1 specimen. [3] A turritellid.
Vermetus V. cornejoi1.5 miles east of Malone station. [3] 8 specimens. [3] A worm shell.

Plants

Fossil remains of plants, including driftwood, are abundant in the Malone Formation, but not well preserved. [1]

See also

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References

  1. 1 2 3 4 5 6 7 8 9 10 May, Steven R.; Bader, Kenneth S.; Boucher, Lisa D.; Jacobs, Louis L.; Lively, Joshua R.; Myers, Timothy S.; Polcyn, Michael J. (2023-06-01). "A record of Late Jurassic vertebrates from Texas". Rocky Mountain Geology. 58 (1): 19–37. doi: 10.24872/rmgjournal.58.1.19 . ISSN   1555-7340.
  2. 1 2 3 Albritton, C. C. (1938-12-01). "Stratigraphy and structure of the Malone Mountains, Texas". Geological Society of America Bulletin. 49 (12_1): 1747–1806. doi:10.1130/GSAB-49-1747. ISSN   0016-7606.
  3. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67 68 69 70 71 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 87 88 89 90 91 92 93 94 95 96 97 98 99 100 101 102 103 104 105 106 107 108 109 110 111 112 113 114 115 116 117 118 119 120 121 122 123 124 125 126 127 128 129 130 131 132 133 134 135 136 137 138 139 140 141 142 143 144 145 146 147 148 149 150 151 152 153 154 155 156 157 158 159 160 161 162 163 164 165 166 167 168 169 170 171 172 173 174 175 176 177 178 179 180 181 182 183 184 185 Cragin, Francis Whittemore (1905). Paleontology of the Malone Jurassic Formation of Texas. Johns Hopkins university.
  4. 1 2 Cooper, Michael; Leanza, Héctor (2019-02-10). "On the Middle Jurassic – Early Cretaceous Megatrigoniinae (Bivalvia, Trigoniida): their biogeography, evolution and classification". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 291 (1): 19–40. doi:10.1127/njgpa/2019/0787. ISSN   0077-7749. S2CID   134666790.