Late Devonian-early Carboniferous ostracods (Crustacea) from South China: taxonomy, diversity and implications
Author
Guillam, Elvis
66D41887-865C-4B91-861F-ADB09B801962
Centre de Recherche en Paléontologie - Paris, MNHN - SU - CNRS; 8 rue Buffon, 75005 Paris, France.
elvis.guillam@sorbonne-universite.fr
Author
Forel, Marie-Béatrice
063C1F7E-6D26-48F9-A8B1-2AFA496B5FB8
Centre de Recherche en Paléontologie - Paris, MNHN - SU - CNRS; 8 rue Buffon, 75005 Paris, France.
marie-beatrice.forel@mnhn.fr
Author
Song, Junjun
5676B30E-AF63-45DE-A465-2EC8BF85ABF9
Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Palaeoenvironment, Chinese Academy of Sciences, Nanjing, China.
jjsong@nigpas.ac.cn
Author
Crasquin, Sylvie
6FDDD550-8522-404D-B3A2-D30BFAA86927
Centre de Recherche en Paléontologie - Paris, MNHN - SU - CNRS; 8 rue Buffon, 75005 Paris, France.
sylvie.crasquin@sorbonne-universite.fr
text
European Journal of Taxonomy
2022
2022-03-15
804
1
62
http://dx.doi.org/10.5852/ejt.2022.804.1689
journal article
55868
10.5852/ejt.2022.804.1689
987c26cd-d47c-4773-8b5a-df53f0eda18e
2118-9773
6359315
5EEDA63F-8A81-40DF-B5A4-C799498DC523
Kloedenellitina spinosa
Gurevitch, 1972
Fig. 6B–C
Kloedenellitina spinosa
Gurevitch, 1972: 333, pl. 11 figs 3–4.
Kloedenellitina spinosa
–
Tschigova 1977: 171
, pl. 41 fig. 13.
Material examined
CHINA
•
1 complete carapace
(♀,
Fig. 6B
);
Blue Snake section
,
Gelaohe Formation
, sample 19BAI 60;
P6M 3857
•
1 complete carapace
(♂,
Fig. 6C
);
Blue Snake section
,
Gelaohe Formation
, sample 19BAI 69;
P6M 3858
•
16 complete carapaces
;
Blue Snake section
,
Gelaohe Formation
, samples 19BAI 60, 19BAI 67–69, 19BAI 74, 19BAI 80.
All from the Famennian
,
late Devonian
.
Dimensions
RV: L = 552–783 µm, H = 307–394µm, H/L = 0.48–0.59.
LV: L = 434–761 µm, H = 210–377 µm, H/L = 0.45–0.56.
Remarks
In the genus
Kloedenellitina
, females have an inflated posterior carapace, which corresponds to a brood pouch (
Ellis & Messina 1964
). This character allows us to distinguish females (
Fig. 6B
) from males (
Fig. 6C
) in the studied material. The lateral surface of the specimens preserving their carapace appears as reticulate (
Fig. 6C
), it is rather smooth in steinkern but the reticulation remains visible in certain areas (
Fig. 6B
). Our material is smaller than the
type
material (L = 760–930 µm, H = 440–490 µm in Gurevitch 1972) with H/L between 0.53 and 0.58 while it is between 0.45 and
0.59 in
our material (both valves taken together). The specimen shown in
Tschigova (1977
: pl. 61 fig. 13) is also larger with L =
1200 mm
, H =
556mm
but the H/L ratio is similar (H/L = 0.46). In the present material, this species may mainly be represented by juvenile specimens corresponding to at least two different ontogenetic stages that we cannot discriminate because of the wide distribution of their dimensions.
Table 2
(continued on next two pages). Stratigraphic distribution of species in the Blue Snake section.
Orange: Association A, Grey: Association B, Green: Association C. |
Gelaohe Formation |
Tangbagou Formation |
Famennian |
latest Fa. |
Tournaisian |
Sample 19BAI Species |
80 |
74 |
69 |
68 |
67 |
63 |
60 |
58 |
55 |
54 |
44 |
43 |
41 |
39 |
37 |
27-2 |
23 |
16 |
08 |
05 |
03 |
02 |
01 |
Knoxina
sp.
|
1 |
8 |
Bairdia nanbiancunensis
|
1 |
2 |
1 |
2 |
Fellerites
sp. 1
|
2 |
1 |
1 |
1 |
3 |
Beyrichiopsis
sp.
|
8 |
1 |
2 |
3 |
1 |
Kloedenellitina spinosa
|
1 |
2 |
2 |
2 |
3 |
1 |
7 |
Kloedenellitina sygmaeformis
|
3 |
2 |
1 |
6 |
3 |
3 |
Knoxiella subcompressa
|
2 |
1 |
2 |
2 |
1 |
Fellerites
sp. 2
|
2 |
2 |
5 |
1 |
1 |
2 |
Knoxiella complanata
|
2 |
1 |
4 |
6 |
2 |
9 |
17 |
5 |
Bairdia hypsela
|
2 |
6 |
1 |
1 |
7 |
1 |
2 |
14 |
2 |
2 |
1 |
9 |
7 |
16 |
3 |
6 |
Parabolbinella
sp.
|
1 |
Sulcella baisuzhena
sp. nov.
|
1 |
1 |
19 |
Clavofabella
?
lanshella
sp. nov.
|
2 |
4 |
17 |
1 |
1 |
Kloedenellitina sincera
|
14 |
1 |
2 |
3 |
Sansabella gelaohensis
sp. nov.
|
73 |
8 |
2 |
3 |
15 |
5 |
Healdianella
sp.
|
1 |
12 |
3 |
7 |
Acratia acutiangulata
|
5 |
15 |
1 |
2 |
4 |
2 |
Bairdia quasikuznecovae
|
1 |
4 |
1 |
2 |
7 |
3 |
1 |
1 |
Acratia
cf.
tschudovoensis
|
1 |
1 |
8 |
1 |
Bairdiacypris nanbiancunensis
|
1 |
1 |
1 |
2 |
3 |
1 |
1 |
2 |
2 |
Clavofabella
? sp.
|
1 |
14 |
Selebratina
sp.
|
1 |
7 |
2 |
Cytherellina caerulea
sp. nov.
|
5 |
4 |
2 |
1 |
Healdianella
cf.
insolita
|
1 |
1 |
1 |
1 |
1 |
Hypotetragona
sp.
|
13 |
12 |
8 |
1 |
3 |
1 |
1 |
1 |
1 |
Bairdia
cf.
susoroides
|
2 |
1 |
2 |
1 |
1 |
Knoxiella
cf.
subcompressa
|
2 |
Cavellina
cf.
dushanensis
|
2 |
1 |
Bairdia semichatovae
|
1 |
6 |
1 |
1 |
Bairdia
(
R
.)
angulatiformis
|
1 |
1 |
3 |
1 |
1 |
1 |
1 |
Table 2
(continued). Stratigraphic distribution of species in the Blue Snake section.
Microcheilinella
cf.
decora
|
8 |
1 |
1 |
2 |
1 |
1 |
1 |
Praepilatina adamszaki
|
1 |
1 |
1 |
2 |
4 |
2 |
2 |
Bairdia obliqua
|
2 |
1 |
2 |
4 |
3 |
6 |
1 |
4 |
1 |
3 |
9 |
2 |
2 |
12 |
10 |
Paraparchites
sp. 2
|
1 |
Cavellina
cf.
recta
|
2 |
Bairdiocypris marginifera
|
1 |
Fabalicypris sundarijanata
|
4 |
2 |
Acratia
cf.
evlanensis
|
1 |
1 |
1 |
3 |
Knoxiella archedensis
|
1 |
1 |
2 |
1 |
4 |
2 |
2 |
8 |
1 |
2 |
Elliptocyprites
sp.
|
1 |
2 |
1 |
1 |
Bairdia
sp. 3
|
2 |
2 |
2 |
Bairdioidea
? indet
|
1 |
1 |
Acratia subobtusa
|
2 |
1 |
2 |
Elliptocyprites lorangeri
|
1 |
Bairdia
cf.
extenuata
Bairdia
(
C
.)
curta
McCoy, 1844
emend. Jones & Kirkby, 1878
in Crasquin, 1986
|
1 1 |
Healdianella faseollina
|
2 |
1 |
Bairdia
sp. 5
|
5 |
1 |
1 |
1 |
1 |
2 |
Healdianella alba
|
1 |
1 |
3 |
2 |
3 |
3 |
2 |
9 |
9 |
9 |
Microcheilinella larionovae
|
1 |
1 |
1 |
1 |
1 |
3 |
1 |
Microcheilinella
sp.
|
4 |
1 |
4 |
3 |
1 |
1 |
3 |
Microcheilinella
sp.
sensu Olempska, 1979
|
1 |
1 |
1 |
3 |
Bairdia
(
R
.) sp. cf.
R
.
sinuosa
(Morey, 1936)
in Crasquin, 1985
|
1 |
5 |
1 |
2 |
1 |
2 |
Healdianella lumbiformis
|
16 |
2 |
1 |
1 |
Bairdiacypris subcyliпdrica
|
33 |
12 |
7 |
1 |
1 |
1 |
2 |
Shishaella hastierensis
|
8 |
2 |
6 |
5 |
5 |
7 |
1 |
7 |
1 |
3 |
2 |
1 |
Bairdia cestriensis
|
1 |
1 |
Shishaella porrecta
|
2 |
1 |
Bairdia submongoliensis
|
1 |
1 |
Bairdia
(
C
.)
laveinei
|
1 |
1 |
1 |
1 |
1 |
Acratia
cf.
insolita
|
1 |
1 |
1 |
1 |
1 |
2 |
1 |
2 |
Acutiangulata
acutiangulata
|
1 |
1 |
3 |
3 |
3 |
2 |
Bairdia mnemonica
|
4 |
2 |
4 |
3 |
2 |
1 |
Bairdia
sp.1
|
2 |
1 |
Bairdia natiformis
|
1 |
1 |
2 |
2 |
1 |
1 |
2 |
Bairdiacypris quasielongata
|
1 |
1 |
1 |
1 |
1 |
3 |
3 |
5 |
Amphissites
sp.
|
2 |
1 |
2 |
5 |
1 |
Table 2
(continued). Stratigraphic distribution of species in the Blue Snake section.
Blessites feluyensis
|
8 |
1 |
8 |
1 |
Bairdia
sp. 6
|
1 |
1 |
1 |
Hypotetragona angulata
|
3 |
4 |
2 |
2 |
1 |
2 |
3 |
7 |
8 |
5 |
Paraparchites longmenshanensis
|
22 |
1 |
2 |
1 |
1 |
1 |
Bairdiocypris fomikhaensis
|
1 |
2 |
1 |
1 |
1 |
1 |
2 |
2 |
5 |
Bairdianella cuspis
|
1 |
1 |
2 |
1 |
3 |
5 |
7 |
6 |
Bairdia
sp. 2
|
2 |
Bairdia solita
|
1 |
4 |
1 |
Microcheilinella
sp.
cf.
M
.
buschminae
Olempska, 1982
in Song & Gong, 2017
|
1 |
1 |
3 |
Coryellina grammi
|
1 |
4 |
1 |
1 |
2 |
1 |
Acratia similaris
|
1 |
2 |
4 |
2 |
4 |
3 |
Acratia
sp.
|
1 |
3 |
3 |
1 |
1 |
1 |
Bairdia
cf.
altifrons
|
1 |
1 |
2 |
Bairdia confragosa
|
3 |
5 |
3 |
2 |
1 |
3 |
10 |
2 |
6 |
Bairdia feliumgibba
|
2 |
6 |
5 |
2 |
7 |
Microcheilinella
sp. A
,
aff.
buschminae
Olempska, 1981
in
Casier et al., 2004
|
1 |
1 |
2 |
Paraparchites
sp. 1
|
1 |
Bairdia
(
R
.)
buschminaae
|
2 |
2 |
Bairdia
(
R
.) cf.
plebeja
|
14 |
1 |
1 |
3 |
2 |
Bairdia
sp. 4
|
1 |
1 |
4 |
6 |
1 |
Bairdia
sp. 7
|
1 |
1 |
Healdianella
cf.
subdistincta
|
2 |
5 |
2 |
1 |
Bairdia
cf.
grahamensis
|
1 |
Bairdia rustica
|
26 |
Bairdiocypris elliptica
|
3 |
2 |
Aparchites
sp.
|
5 |
2 |
1 |
1 |
Acratia
cf.
disjuncta
|
1 |
3 |
Bairdiocypris
sp.
|
1 |
2 |
1 |
2 |
Microcheilinella subrhomboidalis
|
1 |
Microcheilinella infradominica
in
Song & Gong, 2019
|
2 |
2 |
Knoxites
cf.
argulata
|
1 |
1 |
Occurrence
Torchinsk Formation,Volyn region, Russian platform,Tournaisian, early Carboniferous(Gurevitch 1972). Lebedyan horizon, Torchinsk Formation, Central regions of the Russian platform, Famennian, late Devonian (
Tschigova 1977
). Samples 19BAI 60, 19BAI 67–69, 19BAI 74, 19BAI 80, Gelaohe Formation, Blue Snake section, Famennian, late Devonian (this work).