CORALLINE ALGAE FROM THE HUT BAY FORMATION (MIDDLE MIOCENE), LITTLE ANDAMAN, INDIA

被引:0
|
作者
Kishore, S. [1 ]
Jauhri, A. K. [3 ]
Singh, S. K. [4 ]
Malakar, B. [5 ]
Misra, P. K. [2 ]
机构
[1] Rajat PG Coll, Dept Bot, Lucknow, Uttar Pradesh, India
[2] Univ Lucknow, Dept Bot, Lucknow, Uttar Pradesh, India
[3] Univ Lucknow, Dept Geol, Lucknow, Uttar Pradesh, India
[4] Charak Inst Educ, Dept Bot, Lucknow, Uttar Pradesh, India
[5] Pondicherry Cent Univ, Dept Ocean Studies & Marine Biol, Port Blair, India
关键词
Non-geniculate coralline algae; palaeoenvironment; Hut Bay Formation; South Andaman; TAXONOMIC IMPLICATIONS; SOUTHERN SPAIN; RHODOPHYTA; ASSEMBLAGES; PLEISTOCENE; ISLAND; REEF; FORAMINIFERA; PHYLOGENY; REVISION;
D O I
暂无
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
The sediments of Hut Bay Formation (Middle Miocene), Little Andaman are characterized by coralline algae, corals and foraminifera. In the present paper, thirteen species belonging to nine genera of coralline algae are described. Out of these, one species (Harveylithon rupestris) is a new record for India. Eight species (Mesophyllum obsitum, M curium, M koritzae, M. commune, Phymatolithon calcareum, Aethesolithon problematicum, Harveylithon munitum and Sporolithon lvovicum) are first time recorded from the study area. The coralline algal assemblages can be broadly differentiated into two associations: one developed in the lower part of the studied succession deposited in deep, cool-water under low-energy conditions, and the other developed in the upper part indicating deposition in shallow, warm-water with high energy conditions. These two associations along with their growth-forms in the study area suggest that the depth, temperature, and hydrodynamic conditions might have fluctuated during deposition of the Hut Bay Formation. It seems that Lithopyllum and Phymatolithon flourished in relatively cool water environment, while Sporolithon, Harveylithon, Lithoporella, and Aetesolithon might have dominated during the warmer interval.
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页码:205 / 216
页数:12
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