Chara sp.

Sanjuan, Josep & Alqudah, Mohammad, 2018, Charophyte flora from the Miocene of Zahle (Beeka Valley, Lebanon). Biostratigraphic, palaeoenvironmental and palaeobiogeographical implications, Geodiversitas 40 (10), pp. 195-209 : 201-203

publication ID

https://doi.org/ 10.5252/geodiversitas2018v40a10

publication LSID

urn:lsid:zoobank.org:pub:64D30CC3-102C-4A1F-A5AF-C9969BDDDFEE

persistent identifier

https://treatment.plazi.org/id/2F38077C-BC49-FFDE-535E-FAC9216CFB1F

treatment provided by

Marcus

scientific name

Chara sp.
status

 

Chara sp.

( Fig. 3 View FIG I-K)

MATERIAL EXAMINED. — 10 well-preserved gyrogonites have been recovered from sample Zahle 1.

DESCRIPTION Small to medium sized gyrogonites, 486-637 µm high (mean 555 µm) and 375-456µm wide (mean 416µm), elongate and prolate in shape, with an isopolarity index ranging from 120 to 144 (mean 130). Nine to eleven convolutions are visible in lateral view in mean value). Spiral cells flat to concave, about 54 µm wide and without ornamentation. Apex psilocharoid and prominent. Base rounded to slightly pointed showing a small pentagonal basal pore.

REMARKS

This population from Zahle 1 belongs to the genus Chara , although the reduced number of specimens found hinders at present their specific attribution.

Genus Lychnothamnus (Ruprecht, 1845) Leonhardi, 1863 emend. A. Braun in Braun & Nordstedt (1882) Lychnothamnus barbatus (Meyen, 1827) Leonhardi, 1863

Lychnothamnus barbatus var. antiquus Soulié-Märsche, 1989 ( Figs 5 View FIG ; 6 View FIG )

Lychnothamnus barbatus var. antiquus Soulié-Märsche, 1989: 155 , pl. XXXVII, figs 1-6.

MATERIAL EXAMINED. — 40 well-preserved gyrogonites have been recovered from sample Zahle 2.

DESCRIPTION

Gyrogonites large, very variable in size, 619-901µm high (mean 773 µm) and 521-739 µm wide (mean 613 µm), ellipsoidal in shape with an isopolarity index ranging from 108 to 144 (average 125). Spiral cells in the apical zone show a remarkably constant width, which results in a flat apex ( Fig. 5A, B View FIG ). The base is tapered with a star-shaped basal pore, about 80 µm in diameter ( Fig. 5C View FIG ). Nine to eleven (frequently ten) cells visible laterally ( Fig. 5 View FIG D-H). These are normally concave ranging from 62 to 115 µm in height (mean 84 µm), nonornamented and separated by prominent sutures, sometime bicarinated ( Fig. 5D View FIG ).

BIOSTRATIGRAPHY

This species is known from the Miocene in Europe and extends through the Pliocene up to recent times (Soulié- Märshe 1989).

PALAEOECOLOGY

Inferred through comparison with the ecological requirements of its single living representative Lychnothamnus barbatus (check the chapter charophyte palaeoecology).

DISTRIBUTION

Lychnothamnus barbatus var. antiquus has hitherto been recorded from numerous Miocene European localities i.e., Spain (González-Pardos 2012; Suárez-Hernando et al. 2013), southern France (Soulié-Märsche 1989), Portugal (Antunes et al. 1992), Montenegro ( Krstić et al. 2010) and Turkey (Mazzini et al. 2013). The extant representative i.e., L. barbatus is a common species of the moraine lakes of Northern Europe ( Karczmarz 1967). It was formerly known from Germany, Poland, France, Italy and Austria (Migula 1897; Corillion 1972; Krause 1986). Lychnothamnus barbatus has been also recorded in the Balkans area ( Blaženčić et al. 2006), Poland (Sugier et al. 2010) and Ukrainia ( Borisova & Yakushenko 2008). This species has been rarely found growing in other areas out of Europe such as Asia ( Gollerbakh & Krasavina 1983), Australia ( Casanova et al. 2003) and North America ( Karol et al. 2017).

Kingdom

Plantae

Phylum

Charophyta

Class

Charophyceae

Order

Charales

Family

Characeae

Genus

Chara

Loc

Chara sp.

Sanjuan, Josep & Alqudah, Mohammad 2018
2018
Loc

Lychnothamnus barbatus var. antiquus Soulié-Märsche, 1989: 155

Soulie-Marsche 1989: 155
1989
Loc

Lychnothamnus barbatus var. antiquus

Soulie-Marsche 1989
1989
Loc

L. barbatus

Leonhardi 1863
1863
Loc

Lychnothamnus barbatus

Leonhardi 1863
1863
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