Dideroceras glauconiticum (Heinrichson, 1935); Paroistodus originalis Zone, Volkhovian, erratic boulders, Poland. 1. Phragrnocone in ventral (a) and lateral (b) views, ZPAL N /02 5; boulder E- 116, Rozewie. 2. Medial section through a phragmocone, IG 8. H. 265; tile from Opatów. 3. Transverse section through a phragmocone at the mid-length of the specimen, ZPA L N/030; boulder E-116. Rozewie. 4. Medial section through a phragmocone, IG 8. 11. 267; Opatów. 5. Medial section through spiculum of a phragmocone, ZPAL N/039 ; boulder E-228, Międzyzdroje. 6. Transverse section through a phragmocone at the mid-length of the spiculum, ZPAL N/032; boulder E-116. Rozewie. 7. Medial section through spiculum of a phragmocone, ZPAL N/094; boulder E-116, Rozewie. 8. Medial section thr ough spiculum and shell of a phragmocone, IG 8.II.258a, Opatów. 9. Phragmocone in ventral view, IG 8.II. 264, Opatów.
Dideroceras glauconitum ((Heinrichson, 1935); P. originalis Zone, Volkhovian. a. Reconstruction of apical part of thephragrnocone. b-j. Sections through apical part of the shell. b. ZPAL N/032, boulder E-222, Międzyzdroje, Poland; c. IG 8.II.256. d. ZPAL N/031, boulder E-116, Rozewie, Poland. e. IG 8.II.256a. f. ZPAL N/040, boulder E-228, Międzyzdroje. g. ZPAL N/039, same boulder. h. ZPAL N/033, boulder E-116, Rozewie. i. ZPALN/030, same boulder. j. ZPAL N/087, boulder E-I04, Międzyzdroje. k-l. Section through siphuncle IG 8.II.256b and lG 8.II.264.
Diagnoza
Moderately long shell with long air camerae; the length of the septal necks is one third of a chamber length but highly variable; the siphuncle of variable diameter. The spiculum is most commonly drop-like in cross-section, its calcification commenced at the dorsal and lateral sides.
Porównanie
Autekologia
Występowanie geograficzne
Zasięg czasowy
Materiały muzealne
ZPAL, PIG
Literatura
Dzik, J. 1984. Phylogeny of the Nautiloidea. Palaeontologia Polonica 45, 1-255