Well #D-7 (Devonian to of the United States)

Also known as Near Hawarden

Where: Sioux County County, Iowa (43.1° N, 96.4° W: paleocoordinates 29.0° S, 40.1° W)

• coordinate estimated from map

When: Givetian to Givetian (387.7 - 372.2 Ma)

• "a thin, previously unknown deposit of silty shales above a thin sandstone overlying Precambrian gneissic basement and overlain unconformably by the Nishnabotna Member of the Cretaceous Dakota Formation (Ludvigson and Bunker, 1979)."

•“The spores recovered from the Hawarden core are difficult to examine in detail because of the presence of amorphous kerogen in the samples but a Middle or Late Devonian age is suspected (Ravn, personal commun.). A similar unit of brown, sandy, organic-rich shale was encountered approximately 20 km to the east, though not cored, in well D-44, Iowa Geological Survey, Boyden, Sioux County, Iowa (NE/4, SE/4, NE/4 sec. 9, T96N, R44W, Sioux Co.) (Figure 2). Here the shale overlies Cambrian dolomite, probably the Upper Cambrian Bonneterre Formation (Witzke, personal commun.). […] the rocks probably represent the same strati-graphic unit. Palynomorphs present in well D-44, all trilete spores, are relatively free of kerogen and include, most abundantly, Geminospora cf. G. svalbardiae (Vigran, 1964), but also Ver-rucosisporites premnus Richardson, 1965, Dictyotriletes sp., Samarisporites sp., and Convolutispora sp. […] The entire floral assemblage thus seems to indicate a Middle to early Late Devonian, probably Givetian or Frasnian, age (Ravn, personal commun.).”

Environment/lithology: fluvial; pyritic, brown, silty, sandy shale and siltstone

• "The presence of quartzite clasts in the basal sands (Devonian) of the Hawarden core suggests the past existence of fluvial networks draining the ridge. Because of its high local relief, the ridge was probably an island during the maximum extent of the Late Devonian marine transgressions in the area."
• "The unit presents a varve-like, laminated appearance and consists predominantly of light-brown to dark-grey, slightly silty, organic-rich shale, with some fine sand, disseminated pyrite, thin siltstone intercalations, and phosphatic laminae."

Size class: macrofossils

Collection methods: chemical

• "repeatedly processed in household bleach to oxidize the organic shale binder, the residue screened and dried, and systematically picked."

Primary reference: G. W. Storrs. 1987. An ichthyofauna from the subsurface Devonian of northwestern Iowa and its biostratigraphic and paleoecologic significance. Journal of Paleontology 61(2):363-374 [E. Dunne/S. Fasey]more details

Purpose of describing collection: general faunal/floral analysis

PaleoDB collection 226053: authorized by Emma Dunne, entered by Sophie Fasey on 13.06.2022

Creative Commons license: CC BY (attribution)

Taxonomic list

Actinopteri
  -
? Moythomasia sp. Gross 1950
Scales
Osteichthyes
 Osteolepidida - Osteolepididae
Osteolepididae indet. Cope 1887 lobe-finned fish
Scales
 Actinopterygii -
Actinopterygii indet. Cope 1887 ray-finned fish
Jaw and teeth
Placodermi
 Placodermi -
Placodermi indet. armour-plated fish
Bone fragments
Chondrichthyes
 Acanthodiformes - Acanthodidae
"Acanthodes" dublinensis spiny fish
Scales and spines