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首页> 外文期刊>Palaeobotanist >A fossil dicotyledonous wood of Ochnaceae from the Deccan Intertrappean sediments of Mahurzari, Nagpur District, Maharashtra, India
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A fossil dicotyledonous wood of Ochnaceae from the Deccan Intertrappean sediments of Mahurzari, Nagpur District, Maharashtra, India

机译:印度马哈拉施特拉邦那格浦尔区马库扎里德干人际间沉积物中虎杖科植物的双子叶化石

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Ramteke DD & Kapgate DK 2016. A fossil dicotyledonous wood of Ochnaceae from the Deccan Intertrappean sediments of Mahurzari, Nagpur District, Maharashtra, India. The Palaeobotanist 65(2 ): 297-303. The paper describes anatomical details of fossil wood of family Ochnaceae, Ochnaceoxylon tertiera from the Deccan Intertrappean sediments. The wood is preserved in silicified chert from the Deccan Intertrappean beds exposed in a quarry near the village of Mahurzari, India about 14 km from Nagpur (lat. 21°13.280' N, long. 79°0.84' E). The wood described here is silicified measures about 10.5 cm in length and 4.6 cm in diameter. Its detailed anatomy is studied through Transverse Section (T.S.), Tangential Longitudinal Section (T.L.S.) and Radial Longitudinal Section (R.L.S.) planes. The wood is diffuse porous, vessels are mostly solitary and few are in multiples of two to three. Perforation plate is simple and obliquely placed; rays are biseriate to multiseriate and heterogenous, tyloses present. The wood is compared with modern families like Apocynaceae, Dipterocarpaceae, Ochnaceae and Ericaceae. The reported fossil wood shows close resemblance with modern family Ochnaceae. Members of the family Ochnaceae are evergreen, mainly small trees or shrubs, and are presently distributed in tropical and subtropical forests and Savannas. The existence of wood shows the palaeoecological evidence during Maastrichtian.
机译:Ramteke DD&Kapgate DK2016。O科的化石双子叶木材,从印度马哈拉施特拉邦那格浦尔地区的马可扎里德干间带沉积物中提取。古植物学家65(2):297-303。这篇论文描述了来自Deccan Intertrappean沉积物的虎耳草科(Ochnaceoxylon tertiera)的化石木材的解剖学细节。木材保存在位于印度Mahurzari村附近的一座采石场中的Deccan Intertrappean床的硅质硅from石中,该村距那格浦尔约14公里。 21°13.280'N,长。 79°0.84'E)。这里描述的木材是硅化的,长约10.5厘米,直径约4.6厘米。通过横切面(T.S.),切向纵向切面(T.L.S.)和径向纵切面(R.L.S.)平面研究其详细的解剖结构。木材是弥散多孔的,器皿大多是单生的,很少是二至三的倍数。穿孔板简单且倾斜放置;射线是二毛的至多毛的和异种的,酪醇存在。将该木材与夹竹桃科,龙脑香科,龙骨科和蓖麻科等现代家庭进行了比较。报道的化石木材与现代family科科非常相似。 O菜科的成员常绿,主要是小树或灌木,目前分布在热带和亚热带森林和热带稀树草原。木材的存在表明了马斯特里赫特时期的古生态证据。

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