Cylindroniscus flaviae Campos-Filho, Araujo & Taiti, 2017
publication ID |
https://dx.doi.org/10.3897/zookeys.1101.79043 |
publication LSID |
lsid:zoobank.org:pub:CD8B4971-44FE-427C-A246-89090051416D |
persistent identifier |
https://treatment.plazi.org/id/869D6548-8EA8-5F05-BADB-869CADB376EE |
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Cylindroniscus flaviae Campos-Filho, Araujo & Taiti, 2017 |
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Cylindroniscus flaviae Campos-Filho, Araujo & Taiti, 2017
Figs 1 View Figure 1 , 2B View Figure 2
Cylindroniscus flaviae Campos-Filho, Araujo & Taiti, in Campos-Filho et al. 2017a: 229, figs 1-5.
Cylindroniscus flaviae ; Campos-Filho et al. 2017b: 70; Campos-Filho et al. 2018: 4; Fernandes et al. 2018: 441; Silva et al. 2018: 56.
Material examined.
Brazil ● 1♀, Gruta da Tapagem (Caverna do Diabo), Eldorado , Parque Estadual Caverna do Diabo , Açungui geomorphological group, state of São Paulo, 24°38'17.00"S, 48°24'4.00"W, leg. ME Bichuette, T Zepon, JE Gallão, 24.III.2021, LES 27755 View Materials GoogleMaps ● 1♀, same locality and collectors as for preceding, 24.III.2021, LES 27756 View Materials GoogleMaps ● 1♂, 1♀, same locality and collectors as for preceding, 24.III.2021, LES 27757 View Materials GoogleMaps ● 1♀, same locality and collectors as for preceding, 24.III.2021, LES 27758 View Materials GoogleMaps ● 2♀♀, same locality and collectors as for preceding, 24.III.2021, LES 27759 View Materials GoogleMaps ● 1♂, same locality and collectors as for preceding, 25.III.2021, LES 27760 View Materials GoogleMaps .
Remarks.
Cylindroniscus flaviae shows preference for organic matter deposits and highly humid areas in the aphotic zone (Fig. 2B View Figure 2 ). The organic matter was observed in several conduits of the Gruta da Tapagem, always far from the touristic stretches, and it was composed of particulate vegetal debris or small tree branches. The environmental variables along the cave ranged from 19.9 °C to 20.4 °C and the relative air humidity from 95% to 99.1%. The individuals demonstrated sensitivity to the flash lights of the lanterns, always moving in opposite direction.
Distribution.
This species is recorded from several caves in the Açungui geomorphological group (see Campos-Filho et al. 2017).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Cylindroniscus flaviae Campos-Filho, Araujo & Taiti, 2017
Campos-Filho, Ivanklin Soares, Gallo, Jessica S., Gallao, Jonas E., Torres, Dayana F., Carpio-Diaz, Yesenia M., Lopez-Orozco, Carlos Mario, Borja-Arrieta, Ricardo, Taiti, Stefano & Bichuette, Maria Elina 2022 |
Cylindroniscus flaviae
Campos-Filho, Araujo & Taiti 2017 |
Cylindroniscus flaviae
Campos-Filho, Araujo & Taiti 2017 |