<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">IJG</journal-id><journal-title-group><journal-title>International Journal of Geosciences</journal-title></journal-title-group><issn pub-type="epub">2156-8359</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ijg.2023.144017</article-id><article-id pub-id-type="publisher-id">IJG-124411</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Earth&amp;Environmental Sciences</subject></subj-group></article-categories><title-group><article-title>
 
 
  Comprehensive Record of Megafossils from the Rajmahal Basin, Jharkhand, India
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Arun</surname><given-names>Joshi</given-names></name><xref ref-type="aff" rid="aff1"><sub>1</sub></xref></contrib></contrib-group><aff id="aff1"><label>1</label><addr-line>Council of Scientific and Industrial Research (CSIR), New Delhi, India</addr-line></aff><pub-date pub-type="epub"><day>07</day><month>04</month><year>2023</year></pub-date><volume>14</volume><issue>04</issue><fpage>316</fpage><lpage>328</lpage><history><date date-type="received"><day>8,</day>	<month>August</month>	<year>2022</year></date><date date-type="rev-recd"><day>16,</day>	<month>August</month>	<year>2022</year>	</date><date date-type="accepted"><day>21,</day>	<month>April</month>	<year>2023</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  
    The study provides the first comprehensive record of the plant megafossils mainly Glossopteris flora from the Barakar Formation, Rajmahal Open Cast Mine, Rajmahal Basin, Jharkhand. The assemblage is composed of pteridophytes and gymnosperms. The pteridophytes comprise Equisetalean axes (order Equisetales), whereas, gymnosperms include nine species of Glossopteris including
    Glossopteris communis, G. damudica, G. gigas, G. indica, G. lanceolatus, G. longicaulis, G. oldhamii, G. taenioides,
    
   G
   . tenuifolia along
    
   with Vertebraria indica and Noeggerathiopsis hislopi. The present investigation adds to the knowledge of the Glossopteris flora of India, especially that of the Rajmahal Basin from where the plant fossil records are sporadic. The area is a treasure for palaeobotanical studies as evinced by different fossil localities. However, the localities are degraded by mining activities performed by private companies and hence systematic investigation for such vegetation is vital to create a palaeobotanical database before their complete degradation. The floral assemblage compares with earlier known assemblages, recorded from the Barakar Formation of other Lower Gondwana basins of peninsular India. 
  
 
</p></abstract><kwd-group><kwd>Glossopteris Flora</kwd><kwd> Barakar Formation</kwd><kwd> Rajmahal Basin</kwd><kwd> Gondwana</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The Rajmahal Basin covers a large area of Bengal Basin, north Bengal and Purnea Basin. The Basin comprises five coalfields namely Brahmani, Mahuagarhi, Pachwara, Chuperbhita and Hura [<xref ref-type="bibr" rid="scirp.124411-ref1">1</xref>] Megafossils are recorded from different Gondwana basins of India namely Damodar, Mahanadi, Satpura, South Rewa, Wardha, and Godavari basins [<xref ref-type="bibr" rid="scirp.124411-ref2">2</xref>] - [<xref ref-type="bibr" rid="scirp.124411-ref12">12</xref>] but records of these from Rajmahal Basin are scare [<xref ref-type="bibr" rid="scirp.124411-ref13">13</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref14">14</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref15">15</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref16">16</xref>] . No detailed systematic study of megafossils mainly the Glossopteris flora from early Permian has been published so far in the last twenty-five years from Rajmahal Basin. The flora is mainly superintended for the formation of such large reservoirs of coal in the Basin, witnessed by about 10.5 million tons of it from its different coalfields. Hence, it is very necessary to study such coal forming vegetation and its distribution in the other lower Gondwana basins of India. In the present communication, an attempt has been made to study the plant megafossil mainly the Glossopteris flora recovered from the Rajmahal colliery, Rajmahal Basin, Jharkhand India (<xref ref-type="fig" rid="fig1">Figure 1</xref>).</p></sec><sec id="s2"><title>2. Geology of the Area</title><p>The Lower Gondwana exposures are found in the North-South direction of the Rajmahal Basin. The Rajmahal traps capped Rajmahal hills have receded considerably towards the east in the areas towards the north near Ganges, exposing large areas of the coal-bearing Barakar Formation beneath. The Barakars have been identified to be lying with a depositional contact with the Archeans, which lie towards the west. In addition to these lithostratigraphic units, Talchir (underlying the Barakar) and Dubrajpur (underlying the Rajmahal traps) have been exposed in the Basin [<xref ref-type="fig" rid="fig1">Figure 1</xref>(a) &amp; <xref ref-type="fig" rid="fig1">Figure 1</xref>(b)]. The northern part of Hura Coalfield is constituted by Rajmahal Open Cast Mine. The general stratigraphic sequence within the block is given in <xref ref-type="table" rid="table1">Table 1</xref> (after Eastern Coalfields Limited, India).</p></sec><sec id="s3"><title>3. Material and Methods</title><p>Samples were collected from thick carbonaceous shale, Barakar Formation, Rajmahal OCP, Coal Mine Zone-57, Rajmahal Basin (<xref ref-type="fig" rid="fig1">Figure 1</xref>), lies 24˚01'12'' to 25˚01'15'' North latitude and 87˚24'52'' to 87˚25'00'' East longitudes. Impressions of the specimens were studied for their morphotaxonomy with a hand lens and binocular microscope Olympus 20i H under incident light. Taxonomical differences were different leaf shapes, apex, base, margin, midrib and venation patterns. Relevant literature namely [<xref ref-type="bibr" rid="scirp.124411-ref17">17</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref18">18</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] have been consideration for their identification and systematic description. Different species have been recognized on account of taxonomical differences. All the specimens have been deposited in the Botany Department, SGRR (P.G.) College, Dehradun.</p></sec><sec id="s4"><title>4. Result and Discussion</title><p>Systematics</p><p>Division—Pteridophytes</p><p>Order—Equisetales</p><p>Equisetalean axes</p><p>[Plates 1(a)-(c)]</p><p>Description—Seven leafless specimens are in the collection. Their length ranges from 3 to 10 cm and width varies from 0.8 to 4 cm. No nodes are visible in the specimens. However, ridges and furrows can be seen on the axes. 8 - 12 ridges are present and are at a 0.4 to 1.2 mm gap apart from each other.</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> General stratigraphy of the Rajmahal Open Cast Mine, Rajmahal Basin Jharkhand, India (after Eastern Coalfields Limited, India)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  colspan="4"  >STRATIGRAPHIC SEQUENCE OF RAJMAHAL OPEN CAST MINE</th></tr></thead><tr><td align="center" valign="middle" >GROUP</td><td align="center" valign="middle" >FORMATION</td><td align="center" valign="middle" >LITHOLOGY</td><td align="center" valign="middle" >THICKNESS RANGE (m)</td></tr><tr><td align="center" valign="middle" >Recent to Sub-Recent</td><td align="center" valign="middle" >Alluvium</td><td align="center" valign="middle" >-------Unconformity-------</td><td align="center" valign="middle" >0 - 15</td></tr><tr><td align="center" valign="middle" >Upper Gondwana</td><td align="center" valign="middle" >Rajmahal Traps</td><td align="center" valign="middle" >Rajmahal volcanic and intertrappean sandstone and shale ------Unconformity--------</td><td align="center" valign="middle" >50</td></tr><tr><td align="center" valign="middle"  rowspan="3"  >Lower Gondwana</td><td align="center" valign="middle"  rowspan="2"  >Barakar</td><td align="center" valign="middle" >Coarse to medium grained sandstone with shale and coal</td><td align="center" valign="middle" >25 - 350</td></tr><tr><td align="center" valign="middle" >Coarse arkosic sandstone, pebbly at places</td><td align="center" valign="middle" >15 - 150</td></tr><tr><td align="center" valign="middle" >Talchir</td><td align="center" valign="middle" >Sandstones and shales tillites --------Unconformity------- Granite genesis, hornblende Schists and pigmatites</td><td align="center" valign="middle" >10 - 20</td></tr></tbody></table></table-wrap><p>Division—Gymnosperm</p><p>Order—Glossopteridales</p><p>Genus—Glossopteris [<xref ref-type="bibr" rid="scirp.124411-ref20">20</xref>]</p><p>Type species—Glossopteris browniana [<xref ref-type="bibr" rid="scirp.124411-ref20">20</xref>]</p><p>Glossopteris communis [<xref ref-type="bibr" rid="scirp.124411-ref21">21</xref>]</p><p>[Plate 1(d), Plate 1(e)]</p><p>Description—There are twelve specimens in the collection. All the specimens are incomplete. Leaves preserved as impressions, measure 3 -11 cm in length and 2 - 7.2 cm in width at their widest part which is the middle portion of the preserved specimens. Apices are not preserved while the base is tapering in one specimen, the margin is entire. Broad striate midrib is about 3.2 - 4.7 mm wide. The secondary veins arise at angles of about 42˚ - 45˚ from the midrib and after successive dichotomies and anastomoses, form short and broad hexagonal, 4 - 5 mm long and 0.3 - 0.9 mm broad meshes near the midrib, and long and narrow meshes 4 - 6 mm long and 0.1 - 0.5 mm broad near the margin. The vein density is 15 - 17 per cm near the midrib and 22 - 27 per cm near the margin.</p><p>Remarks—Leaves are identical to G. communis [<xref ref-type="bibr" rid="scirp.124411-ref22">22</xref>] pl. 21, fig. 5; [<xref ref-type="bibr" rid="scirp.124411-ref23">23</xref>] pl. 17, figs. 1-2; [<xref ref-type="bibr" rid="scirp.124411-ref24">24</xref>] pl. 21, figs 13-14; [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 1, figs 2-3; [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 3, fig. 1 in venation pattern.</p><p>Glossopteris damudica [<xref ref-type="bibr" rid="scirp.124411-ref23">23</xref>]</p><p>[Plate 1(f)]</p><p>Description—Two incomplete leaf impressions are present in the collection. Leaves measure 6 - 9 cm in length and 5 - 5.6 cm in width at their widest which is the middle part. Leaves elliptical in shape with entire margin, apices and bases are not preserved. Midrib distinct, striate (2 - 3 striations) and 2 - 3 mm broad. Secondary veins arise at angles of 40˚ - 45˚ from the midrib, arch and meet the margin at angles of about 65˚ - 75˚. Meshes are hexagonal in shape, broad and long near midrib (4 - 5 mm long and 0.5 - 1 mm broad) and small and narrower near the margin (1.5 - 2 mm long and 0.2 - 0.6 mm broad). 12 - 16 veins per cm present near midrib and 17 - 22 per cm near at margin.</p><p>Remarks—Present specimens are similar to Glossopteris damudica [<xref ref-type="bibr" rid="scirp.124411-ref23">23</xref>] pl. 20, fig. 2, pl. 31, figs. 1-3, pl. 32, fig. 1; [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 6, fig. 5; [<xref ref-type="bibr" rid="scirp.124411-ref9">9</xref>] figs 6 C, D; [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 3, fig. 3 in presence of broad midrib and polygonal meshes.</p><p>Glossopteris gigas [<xref ref-type="bibr" rid="scirp.124411-ref25">25</xref>]</p><p>[Plate 1(g)]</p><p>Description—There are three leaves in the collection. Leaves range from 4 - 16.6 cm in length and 5 - 10 cm in width at their widest which is generally the middle portion of the leaves. Absence of the apex and base, however, margin entire. Broad striate midrib about 2.5 - 5.2 mm wide at the lower part while 1.7 - 3 mm wide at the upper part. The secondary veins arise at angles of about 45˚ - 50˚ from the midrib and after a short distance, arch and meet the margin at angles of about 75˚ - 85˚. Hexagonal meshes about 3 - 4 mm long and 0.5 - 1 mm broad are found in the specimens. The vein density is 14 - 16 per cm near midrib and 18 - 20 per cm towards the margin.</p><p>Remark—The specimens are similar to Glossopteris gigas described by [<xref ref-type="bibr" rid="scirp.124411-ref25">25</xref>] pl. 3, figs 10, 14, text-fig. 2B), [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 12, fig. 1, pl. 16, fig. 6, pl. 25, fig. 1, [<xref ref-type="bibr" rid="scirp.124411-ref26">26</xref>] pl. 2, fig. 3, pl. 3, fig. 2 and [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 3, figs 4-5 in general shape, midrib and venation pattern.</p><p>Glossopteris indica [<xref ref-type="bibr" rid="scirp.124411-ref27">27</xref>]</p><p>[Plate 1(h), Plate 1(i); Plate 2(a)]</p><p>Description—Fourteen specimens are in the collection. Leaves are lanceolate in shape with an entire margin. Acute apex is present in well preserved specimens. Leaves are 7 - 23 cm long and 3 - 5.2 cm broad at their widest part. Distinct, persistent and striate midrib with 3 - 5 deep striations and 1 - 3 mm wide present in the specimens. The secondary veins arise at angles of about 40˚ - 45˚ from the midrib and after successive dichotomies and anastomoses form polygonal, short and broad meshes near the midrib and narrow–elongate meshes near the margin. The secondary veins arise at an angle of 67˚ - 73˚. Meshes are 1 - 4 mm in length and 0.2 - 0.4 mm in width near midrib and 2.2 - 3.7 mm lengthwise and 0.3 - 0.5 mm in breath at the margin. 16 - 20 veins per cm are present near midrib and 18 - 26 per cm near the margin.</p><p>Remarks—Specimens are alike Glossopteris indica [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 5, fig. 1, pl. 10, fig. 4, pl. 15, fig. 11, pl. 28, fig. 1, pl. 29, fig. 1; [<xref ref-type="bibr" rid="scirp.124411-ref26">26</xref>] pl. 1, fig. 4; [<xref ref-type="bibr" rid="scirp.124411-ref27">27</xref>] pl. 4, fig. 4 and [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 4, figs. 1-2 in shape, nature of midrib and venation pattern.</p><p>Glossopteris lanceolatus [<xref ref-type="bibr" rid="scirp.124411-ref25">25</xref>]</p><p>[Plate 2(b), Plate 2(c)]</p><p>Description—There are three leaf specimens in the collection. Leaves narrow, oblong in shape, measures 7 - 12.2 cm in length and 3 - 4 cm in width, apex acute, base absent and margin slightly undulating. 0.7 mm broad striate midrib is present and gradually gets tapers towards apex. Secondary veins arise at about 45˚ from midrib and after dichotomization and anastomoses, meet the margin at about 85˚. Meshes broad, elongate, 3.5 - 5 mm in length and 0.5 - 0.6 mm wide are present near the midrib while narrow about 2 - 2.5 mm long and 0.3 - 0.4 mm broad near the margin. 17 - 22 veins per cm are present near midrib and 24 - 31 per cm near the margin.</p><p>Remarks—Present specimens are similar with G. lanceolatus delineated by [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 7, fig. 2, pl. 19, fig. 2, pl. 40, fig. 2 and [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 4, fig. 3 in similar shape and venation pattern.</p><disp-formula id="scirp.124411-formula1"><graphic  xlink:href="//html.scirp.org/file/2-2802240x3.png?20230428174906500"  xlink:type="simple"/></disp-formula><p>Plate 1. Scale bar = 1 cm. (a)-(c): Equisetalean axes, specimens nos. RJ 1/2017, RJ 2/2019 and RJ 3/2019. (d) (e): Glossopteris communis, specimens nos. RJ 4/2019 and RJ 5/2019. (f). Glossopteris damudica, specimen no. RJ 6/2019. (g): Glossopteris gigas, specimen no. RJ 7/2019. (h) (i): Glossopteris indica, specimens nos. RJ 8/2019 and RJ 9/2019.</p><p>Glossopteris longicaulis [<xref ref-type="bibr" rid="scirp.124411-ref23">23</xref>]</p><p>[Plate 2(d)]</p><p>Description—There are five incomplete leaf impressions in the collection, which measure 8 - 12 cm in length and 3 - 4.5 cm in width at their widest, margin entire, midrib strong, elevated and 3 mm broad. Leaves are characterized by long, narrow petiole, measuring about 1.5 - 2 cm in length. Secondary veins angle of arise is about 47˚ - 52˚ from midrib. Meshes are polygonal in shape, short and broad, 2 - 3 mm long and 0.5 - 1 mm broad near midrib, long and narrow, 3 - 4 mm long and 0.5 mm broad near margin. The vein density is 13 - 15 per cm near midrib and 16 - 18 per cm near the margin.</p><p>Remarks—The present specimen bear resemblance to Glossopteris longicaulis [<xref ref-type="bibr" rid="scirp.124411-ref24">24</xref>] pl. 31, figs 1-3; [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 1, fig. 4, pl. 15, fig. 13; [<xref ref-type="bibr" rid="scirp.124411-ref30">30</xref>] pl. 1, fig. 5; [<xref ref-type="bibr" rid="scirp.124411-ref27">27</xref>] pl. 4, fig. 8 and [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 4, figs 4-5 [<xref ref-type="bibr" rid="scirp.124411-ref26">26</xref>] in presence of petiole, nature of midrib and in venation pattern.</p><p>Glossopteris oldhamii [<xref ref-type="bibr" rid="scirp.124411-ref31">31</xref>]</p><p>[Plate 2(e), Plate 2(f)]</p><p>Description—Two incomplete leaf impressions are present in the collection. Leaves are 7.1 - 7.3 cm lengthwise and 3.7 - 4.5 cm widthwise. Acute apices and bases are absent. Secondary veins angle is 42˚ - 47˚ from the midrib, arch backwards and run straight upto the margin. Meshes are borad near midrib and narrower towards the margin with 3.3 - 4.7 mm in length and 0.5 - 0.7 mm in near midrib while, 6.2 - 7.7 mm in length and 0.3 - 0.4 mm in width towards margin. Vein density is 22 - 27 per cm near the midrib and 19 - 24 per cm near the margin.</p><p>Remarks—Present specimens are identical to G. oldhamii described by [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 8, fig. 3, pl. 19, fig. 9, pl. 37, fig. 1, [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 4, fig. 8, pl. 5, fig. 1 in similar shape and venation pattern.</p><p>Glossopteris taenioides [<xref ref-type="bibr" rid="scirp.124411-ref23">23</xref>]</p><p>(Plate 2(g); Plate 3(a))</p><p>Description—There are three incomplete specimens in the collection. Preserved portions of the specimens measure 3.1 to 4 cm in length and 0.5 to 1 cm in width in the middle part. Ribbon like leaves have an entire margin, acute apex and base absent. There is distinct, broad and striate midrib of about 1.1 mm wide at lower and 0.5 mm broad at the apex present in the specimens. The secondary veins arise from midrib at angles of about 50˚ - 55˚ and after successive dichotomies, meet the margin at an angle of about 90˚. The shape of meshes is arcuate near the midrib and mostly trapezoid elsewhere. Short and broad meshes are present, they are 2.2 - 3.4 mm in length and 0.3 - 1.2 mm in width towards midrib and narrow about 3.1 - 4.3 mm long and 0.4 - 0.6 mm broad near margin. The vein density is 16 - 20 per cm near midrib and 22 - 26 per cm near the margin.</p><p>Remarks—The present specimens are resemble with Glossopteris taenioides described by [<xref ref-type="bibr" rid="scirp.124411-ref23">23</xref>] pl. 21, fig. 4; [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 4, fig. 6, pl. 18, fig. 5, pl. 43, fig. 3, text–figs 26 D, d and [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 5, fig. 5 in narrow, oblong, ribbon–like shape, broad and strong midrib and venation pattern.</p><p>Glossopteris tenuifolia [<xref ref-type="bibr" rid="scirp.124411-ref32">32</xref>]</p><p>[Plate 3(b), Plate 3(c)]</p><p>Description—Four incomplete specimens are present in the collection, preserved portions measure 7 - 9.4 cm in length and 1.2 - 1.5 cm in width at their widest part. Leaves are linear in shape with entire margin, apex and base are not preserved. Midrib broad, strong, elevated with striations (3 - 4 striations). The secondary veins arise at angles of about 40˚ - 45˚, slightly arch backwards and</p><disp-formula id="scirp.124411-formula2"><graphic  xlink:href="//html.scirp.org/file/2-2802240x4.png?20230428174906500"  xlink:type="simple"/></disp-formula><p>Plate 2. Scale bar = 1 cm. (a) Glossopteris indica, specimen no. RJ 10/2019. (b) (c): Glossopteris lanceolatus, specimens nos. RJ 11/2019 and RJ 12/2019. (d): Glossopteris longicaulis, specimen no. RJ 13/2019. (e) (f): Glossopteris oldhamii, specimens nos. RJ 14/2019 and RJ 15/2019. (g): Glossopteris taneioides, specimen no. RJ 16/2019.</p><p>meet the margin at angles of about 70˚ - 75˚ after dichotomizing and anastomosing, meshes narrow, elongate and hexagonal in shape. The vein density is 19 - 22 per cm near the midrib and 23 - 25 per cm near the margin.</p><p>Remarks—Present leaves are identical to Glossopteris tenuifolia [<xref ref-type="bibr" rid="scirp.124411-ref32">32</xref>] pl. 20, fig. 14, pl. 21, fig. 15, text-fig. 2; [<xref ref-type="bibr" rid="scirp.124411-ref19">19</xref>] pl. 6, figs. 1-2, pl. 15, fig. 10, pl. 17, fig. 10, pl. 42, figs. 1, 6; [<xref ref-type="bibr" rid="scirp.124411-ref30">30</xref>] pl. 1, fig. 5; [<xref ref-type="bibr" rid="scirp.124411-ref26">26</xref>] pl. 2, figs 4-5, pl. 4, fig. 1; [<xref ref-type="bibr" rid="scirp.124411-ref29">29</xref>] pl. 2, figs 5, 9, pl. 3, fig. 4, pl. 4, fig. 5; [<xref ref-type="bibr" rid="scirp.124411-ref9">9</xref>] figs 7 C, D; [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 5, figs. 6-8 ) in shape and venation pattern.</p><p>Genus—Vertebraria [<xref ref-type="bibr" rid="scirp.124411-ref33">33</xref>]</p><p>Type species—Vertebraria australis [<xref ref-type="bibr" rid="scirp.124411-ref33">33</xref>]</p><p>Vertebraria indica</p><p>[Plate 3(d)]</p><p>Description—There are seventeen incomplete horizontally preserved unbranched specimens in the collection. Their size ranges from 2 - 15 cm in length and 0.5 - 3.5 cm in width. Axes consist of 4 to 12 rectangular areas, arranged in linear rows. These rectangular areas are not of equal size and a longitudinal median ridge is present in between the rows of rectangular area. These rectangular areas are separated by a median groove which is 1.4 - 4 mm broad.</p><p>Remarks—The specimens compare in their morphological features with Vertebraria indica [<xref ref-type="bibr" rid="scirp.124411-ref36">36</xref>] pl. 1, figs 3, 4 and 9; [<xref ref-type="bibr" rid="scirp.124411-ref5">5</xref>] fig. 1 a, b; [<xref ref-type="bibr" rid="scirp.124411-ref37">37</xref>] fig. 3 a-d; [<xref ref-type="bibr" rid="scirp.124411-ref6">6</xref>] fig. 3 e-g; [<xref ref-type="bibr" rid="scirp.124411-ref1">1</xref>] pl. 1, figs. 3-5.</p><p>Genus—Noeggerathiopsis [<xref ref-type="bibr" rid="scirp.124411-ref21">21</xref>]</p><p>Type species—Noeggerathiopsis hislopi [<xref ref-type="bibr" rid="scirp.124411-ref22">22</xref>]</p><p>Noeggerathiopsis hislopi [<xref ref-type="bibr" rid="scirp.124411-ref22">22</xref>]</p><p>[Plate 3(e)]</p><p>Description—Two leaves are present in the collection. The leaf is broad at the upper end. Size of the leaves ranges from 4 to 15 cm in length and 0.4 to 1.8 cm in width at base and 1.6 to 2.4 cm in width near apex. Veins arise from base, run parallel for a very short distance of about 0.7 to 1 cm, divert at angles of about 5˚ - 7˚ to meet the margin. The primary veins dichotomize toward upper part to form secondary veins. The vein density near the leaf base is 10 - 12 per cm and 12 - 16 per cm near the apex.</p><p>Remarks—The present specimen bear resemblance to Noeggerathiopsis hislopi [<xref ref-type="bibr" rid="scirp.124411-ref22">22</xref>] pl. 19, fig. 5, pl. 19, figs 1-6, pl. 20, fig. 1; [<xref ref-type="bibr" rid="scirp.124411-ref38">38</xref>] pl. 1, figs 1-3; [<xref ref-type="bibr" rid="scirp.124411-ref39">39</xref>] pl. 1, figs. 1-3; [<xref ref-type="bibr" rid="scirp.124411-ref11">11</xref>] pl. 6, figs 2, 3 in dichotomizing parallel veins.</p></sec><sec id="s5"><title>5. Conclusion</title><p>The present study reveals that the area is rich in Glossopteris flora as about nine species of Glossopteris recovered along with Equisetalean axes, Vertebraria indica and Noeggerathiopsis hislopi. Out of nine species of Glossopteris (<xref ref-type="table" rid="table2">Table 2</xref>), five species (namely Glossopteris gigas, G. lanceolatus, G. longicaulis, G. taenioides and G. tenuifolia) are first time documented here from the Basin, especially from Coal Mine Zone-57, Rajmahal colliery, Jharkhand. The occurrence of Vertebraria indica in abundance represents its autochthonous deposition and flushing environment better suited for the growth and development of the flora within the vicinity [<xref ref-type="bibr" rid="scirp.124411-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref36">36</xref>] . The occurrence of both wide and narrow leaves specimens endorse a phase of transition from Lower to Upper Barakar. Besides, it is</p><disp-formula id="scirp.124411-formula3"><graphic  xlink:href="//html.scirp.org/file/2-2802240x5.png?20230428174906500"  xlink:type="simple"/></disp-formula><p>Plate 3. Scale bar = 1 cm. (a) Glossopteris taenioides, specimen no. RJ 17/2019; (b) (c): Glossopteris tenuifolia, specimens nos. RJ 18/2019 and RJ 19/2019; (d): Vertebraria indica, specimen no. RJ 20/2019; (e): Noeggerathiopsis hislpoi, specimen no. RJ 21/2019.</p><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Distribution of plant fossil taxa (present study) of Rajmahal Open Cast Mine in the Barakar Formation of other lower Gondwana basins of India</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Name of Taxa</th><th align="center" valign="middle"  colspan="6"  >Lower Gondwana basins of India</th></tr></thead><tr><td align="center" valign="middle" >Damodar</td><td align="center" valign="middle" >Mahanadi</td><td align="center" valign="middle" >Wardha</td><td align="center" valign="middle" >Satpura</td><td align="center" valign="middle" >South Rewa</td><td align="center" valign="middle" >Godavari Graben</td></tr><tr><td align="center" valign="middle" >Equisetalean axes</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >Glossopteris communis</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >Glossopteris damudica</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >*Glossopteris gigas</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >Glossopteris indica</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >*Glossopteris lanceolatus</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >*Glossopteris longicaulis</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >Glossopteris oldhamii</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >*Glossopteris taenioides</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >*Glossopteris tenuifolia</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >Vertebraria indica</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >-</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr><tr><td align="center" valign="middle" >Noeggerathiopsis hislopi</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td><td align="center" valign="middle" >+</td></tr></tbody></table></table-wrap><p>*New records from the Area.</p><p>representing large floral diversity within the vicinity during their deposition and advocates for favourable environmental conditions for the development of such luxuriant Glossopteris vegetation [<xref ref-type="bibr" rid="scirp.124411-ref40">40</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref41">41</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref42">42</xref>] [<xref ref-type="bibr" rid="scirp.124411-ref43">43</xref>] . The floral assemblage represents dense coal forming vegetation, responsible for the formation of large coal reservoirs in the area. The study helps to record a new palaeobotanical database of such coal forming vegetation before its devastation due to unplanned mining activities. As the government of Jharkhand has given mining leases to private companies, these companies are running in an unplanned manner. Therefore more efforts are needed to study such coal forming vegetation and its distribution for the generation of new palaeobotanical records from the area. The record will surely be helpful to understand the diversity of plants and palaeoenvironment precisely during the deposition of the Barakar Formation in the area.</p></sec><sec id="s6"><title>Acknowledgements</title><p>Author sincerely thanks to Council of Scientific and Industrial Research (CSIR), India for giving financial assistance under project 13(9125-A)/2019-Pool. Warm gratitude towards the Eastern Coalfield Limited administration for giving permission to visit the colliery and for their kind help during the field trip and the Principal, S.G.R.R. (P.G.) College, Dehradun for providing necessary facilities to carried out the research work.</p></sec><sec id="s7"><title>Conflicts of Interest</title><p>Author states that there is no conflict of interest.</p></sec><sec id="s8"><title>Cite this paper</title><p>Joshi, A. (2023) Comprehensive Record of Megafossils from the Rajmahal Basin, Jharkhand, India. International Journal of Geosciences, 14, 316-328. https://doi.org/10.4236/ijg.2023.144017</p></sec></body><back><ref-list><title>References</title><ref id="scirp.124411-ref1"><label>1</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Joshi</surname><given-names> A. </given-names></name>,<etal>et al</etal>. (<year>2018</year>)<article-title>In Situ Occurrence of Vertebrariaindica from the Rajmahal Open Cast Mine, Rajmahal Basin, India: An Evidence for Coal Forming Vegetation</article-title><source> Journal of Terrestrial and Marine Research</source><volume> 2</volume>,<fpage> 12</fpage>-<lpage>16</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.124411-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">Lakhanpal, R.N., Maheshwari, H.K. and Awasthi, N. (1976) A Catalogue of Indian Fossil Plants. Birbal Sahni Institute of Palaeobotany, Lucknow.</mixed-citation></ref><ref id="scirp.124411-ref3"><label>3</label><mixed-citation publication-type="other" xlink:type="simple">Chandra, S. and Tewari, R. (1991) A catalogue of Fossil Plants from India—B. Palaeozoic and Mesozoic Megafossils. Part 2, Birbal Sahni Institute of Palaeobotany, Lucknow.</mixed-citation></ref><ref id="scirp.124411-ref4"><label>4</label><mixed-citation publication-type="other" xlink:type="simple">Srivastava, A.K. (1992) Plant Fossil Assemblages from the Barakar Formation of Raniganj Coalfield, India. Journal of Palaeosciences, 39, 281-302. https://doi.org/10.54991/jop.1990.1695</mixed-citation></ref><ref id="scirp.124411-ref5"><label>5</label><mixed-citation publication-type="other" xlink:type="simple">Singh, K.J. and Chandra, S. (1995) In Situ Preserved Vertebraria Axes in Ib River Coalfield, India. Current Science, 69, 228-229.</mixed-citation></ref><ref id="scirp.124411-ref6"><label>6</label><mixed-citation publication-type="other" xlink:type="simple">Singh, K.J., Saxena, A. and Goswami, S. (2016) In Situ Occurrence of Vertebraria Roots in the Raniganj Formation of Singrauli Coalfield and Its Palaeoecological Significance. Current Science, 110, 299-301.</mixed-citation></ref><ref id="scirp.124411-ref7"><label>7</label><mixed-citation publication-type="other" xlink:type="simple">Singh, K.J., Goswami, S. and Srivastava, G. (2011) Palaeodiversity in the Genus Glossopteris from the Lower Gondwana Rocks of the Korba Coalfield, Chhattisgarh State, India. Journal of Paleontological Society of India, 56, 45-64.</mixed-citation></ref><ref id="scirp.124411-ref8"><label>8</label><mixed-citation publication-type="other" xlink:type="simple">Srivastva, A.K. and Agnihotri, D. (2009) Palaeobotanical Perspectives of Satpura Gondwana Basin, Madhya Pradesh. Earth System Sciences, 2, 581-595.</mixed-citation></ref><ref id="scirp.124411-ref9"><label>9</label><mixed-citation publication-type="other" xlink:type="simple">Tewari, R., Pandita, S.K., Agnihotri, D, Pillai, S.S.K. and Bernardes-de-Oliveira, M.E.C. (2012) An Early Permian Glossopteris Flora from the Umrer Coalfield, Wardha Basin, Maharashtra, India. Alcheringa, 36, 355-371. https://doi.org/10.1080/03115518.2012.648416</mixed-citation></ref><ref id="scirp.124411-ref10"><label>10</label><mixed-citation publication-type="other" xlink:type="simple">Joshi, A., Tewari, R. and Agnihotri, D. (2014) Plant Diversity in the Kamthi Formation of India: A Review. Journal of Palaeosciences, 63, 127-136. https://doi.org/10.54991/jop.2014.328</mixed-citation></ref><ref id="scirp.124411-ref11"><label>11</label><mixed-citation publication-type="other" xlink:type="simple">Tewari, R., Joshi, A. and Agnihotri, D. (2017) The Glossopteris Flora of Manuguru Area, Godavari Graben, Telangana, India. Journal of Palaeosciences, 66, 17-36. https://doi.org/10.54991/jop.2017.276</mixed-citation></ref><ref id="scirp.124411-ref12"><label>12</label><mixed-citation publication-type="other" xlink:type="simple">Joshi, A. (2016) The Glossopteris Flora of Manuguru Area, Godavari Graben: Palaeoecological Implications, Evolutionary Perspectives and Basinal Correlation. Ph.D. Thesis, H.N.B. Garhwal University, Srinagar.</mixed-citation></ref><ref id="scirp.124411-ref13"><label>13</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Ball</surname><given-names> V. </given-names></name>,<etal>et al</etal>. (<year>1877</year>)<article-title>Geology of Rajmahal Hills</article-title><source> Memoirs of the Geological Survey of India</source><volume> 13</volume>,<fpage> 1</fpage>-<lpage>94</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.124411-ref14"><label>14</label><mixed-citation publication-type="other" xlink:type="simple">Maheshwari, H.K. and Prakash, G. (1965) Studies in the Glossopteris Flora of India-21. Plant Megafossils from the Lower Gondwana Exposures along Bansloi River in Rajmahal Hills, Bihar. Journal of Palaeosciences, 13, 115-128. https://doi.org/10.54991/jop.1964.687</mixed-citation></ref><ref id="scirp.124411-ref15"><label>15</label><mixed-citation publication-type="other" xlink:type="simple">Prasad, B., Shukla, V.D. and Maithy, P.K. (1987) Megafossils of the Lower Gondwana Succession in Pachhwara Coalfield, Bihar. Gondwana Geological Magzine, 2, 17-29.</mixed-citation></ref><ref id="scirp.124411-ref16"><label>16</label><mixed-citation publication-type="other" xlink:type="simple">Maheshwari, H.K. and Bajpai, U. (1992) Ginkgophyte Leaves from the Permian Gondwana of Rajmahal Basin. Palaeontographica Abteilung B, 224, 131-149.</mixed-citation></ref><ref id="scirp.124411-ref17"><label>17</label><mixed-citation publication-type="other" xlink:type="simple">Lawrence, G.H.M. (1955) An Introduction to Plant Taxonomy. The Macmillan Company, New York, 179.</mixed-citation></ref><ref id="scirp.124411-ref18"><label>18</label><mixed-citation publication-type="other" xlink:type="simple">Melville, R. (1969) Leaf Venation Patterns and the Origin of the Angiosperms. Nature, 224, 121-125. https://doi.org/10.1038/224121a0</mixed-citation></ref><ref id="scirp.124411-ref19"><label>19</label><mixed-citation publication-type="other" xlink:type="simple">Chandra, S. and Surange, K.R. (1979) Revision of the Indian Species of Glossopteris. Birbal Sahni Institute of Palaeobotany, Lucknow.</mixed-citation></ref><ref id="scirp.124411-ref20"><label>20</label><mixed-citation publication-type="other" xlink:type="simple">Brongniart, A. (1828) Histoire des vegetaux fossils, ou, recherches botaniques sur les vegetaux renfermes dans les diverses couches du globe. Paris, 1, 136 p.https://doi.org/10.5962/bhl.title.60992</mixed-citation></ref><ref id="scirp.124411-ref21"><label>21</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Feistmantel</surname><given-names> O. </given-names></name>,<etal>et al</etal>. (<year>1876</year>)<article-title>Notes on the Age of some Fossil Floras in India—VII. Flora of the Jabalpur Group in South Rewah, Near Jabalpur, and in the Satpura Basin</article-title><source> Records of the Geological Survey of India</source><volume> 9</volume>,<fpage> 125</fpage>-<lpage>129</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.124411-ref22"><label>22</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Feistmantel</surname><given-names> O. </given-names></name>,<etal>et al</etal>. (<year>1879</year>)<article-title>The Fossil Flora of Lower Gondwana—The Flora of Talchir–Karharbari Beds</article-title><source> Memoirs of the Geological Survey of India</source><volume> 12</volume>,<fpage> 1</fpage>-<lpage>48</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.124411-ref23"><label>23</label><mixed-citation publication-type="other" xlink:type="simple">Feistmantel, O. (1882) The Fossil Flora of the Gondwana System in India—1. The Fossil Flora of the South Rewah Gondwana Basin. Memoirs of the Geological Survey of India, 12, 3(4), 52 p.</mixed-citation></ref><ref id="scirp.124411-ref24"><label>24</label><mixed-citation publication-type="other" xlink:type="simple">Feistmantel, O. (1880) The Fossil Flora of Gondwana System (Lower Gondwana). II. The Flora of Damuda-Panchet Division. Memoirs of Geological Survey of India: Palaeotonlogia Indica, 12, 77.</mixed-citation></ref><ref id="scirp.124411-ref25"><label>25</label><mixed-citation publication-type="other" xlink:type="simple">Pant, D.D. and Singh, K.B. (1971) Cuticular Structure of Some Indian Lower Gondwana Species of Glossopteris Brongniart Part III. Palaeontographica Abteilung B, 135, 1-40.</mixed-citation></ref><ref id="scirp.124411-ref26"><label>26</label><mixed-citation publication-type="other" xlink:type="simple">Tewari, R. (2007) The Glossopteris Flora from the Kamptee Coalfield, Wardha Basin, Maharashtra, India. Palaeontographica Abteilung B, 277, 43-64. https://doi.org/10.1127/palb/277/2007/43</mixed-citation></ref><ref id="scirp.124411-ref27"><label>27</label><mixed-citation publication-type="other" xlink:type="simple">Schimper, W.P. (1869) Traité de paléontologie végétale. Vol. 1, J.B. Bailliere et Fils, Paris, 738.</mixed-citation></ref><ref id="scirp.124411-ref28"><label>28</label><mixed-citation publication-type="other" xlink:type="simple">Tewari, R. and Srivastava, A.K. (2000a) Plant Fossils Assemblage from the Talchir Formation, Auranga Coalfield, Bihar, India. Journal of Palaeosciences, 49, 23-30. https://doi.org/10.54991/jop.2000.129</mixed-citation></ref><ref id="scirp.124411-ref29"><label>29</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Tewari</surname><given-names> R. </given-names></name>,<etal>et al</etal>. (<year>2008</year>)<article-title>The Genus Glossopteris Brongniart from the Kamthi Formation of Camp IV Area, Wardha Valley Coalfield, Wardha Basin, Maharashtra, India</article-title><source> Journal of Palaeontological Society of India</source><volume> 53</volume>,<fpage> 19</fpage>-<lpage>30</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.124411-ref30"><label>30</label><mixed-citation publication-type="other" xlink:type="simple">Tewari, R. and Srivastava, A.K. (2000b) Plant Fossils from Bhareli Formation of Arunachal Pradesh, North-East Himalaya, India. Journal of Palaeosciences, 49, 209-218. https://doi.org/10.54991/jop.2000.142</mixed-citation></ref><ref id="scirp.124411-ref31"><label>31</label><mixed-citation publication-type="other" xlink:type="simple">Pant, D.D. and Singh, R.S. (1974) On the Stem attacHment of Glossopteris and Gangamopteris Leaves, Part 2, Structural Features. Palaeontographica Abteilung B, 147, 42-73.</mixed-citation></ref><ref id="scirp.124411-ref32"><label>32</label><mixed-citation publication-type="other" xlink:type="simple">Pant, D.D. and Gupta, K.L. (1968) Cuticular Structure of Some Indian Lower Gondwana Species of Glossopteris Brongniart. Part 1. Palaeontographica Abteilung B, 124, 45-81.</mixed-citation></ref><ref id="scirp.124411-ref33"><label>33</label><mixed-citation publication-type="other" xlink:type="simple">McCoy, F. (1847) On the Fossil Botany and Zoology of Rocks Associated with the Coal of Australia. Annals and Magazine of Natural History, 20, 298-312. https://doi.org/10.1080/037454809496054</mixed-citation></ref><ref id="scirp.124411-ref34"><label>34</label><mixed-citation publication-type="other" xlink:type="simple">Royle, J.F. (1833-1839) Illustrations of the Botany and Other Branches of Natural History of the Himalayan Mountains, and of the Flora of Cashmere. Wm. H. Allen, London. https://doi.org/10.5962/bhl.title.449</mixed-citation></ref><ref id="scirp.124411-ref35"><label>35</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Feistmantel</surname><given-names> O. </given-names></name>,<etal>et al</etal>. (<year>1877</year>)<article-title>Notes on Fossil Floras in India XI. Note on Plant Fossils from Barakar District (Barakar Group)</article-title><source> Records of Geological Survey of India</source><volume> 10</volume>,<fpage> 73</fpage>-<lpage>74</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.124411-ref36"><label>36</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Srivastava</surname><given-names> A.K. </given-names></name>,<etal>et al</etal>. (<year>1995</year>)<article-title>Nature and Preservation of Vertebraria Axes in the Lower Gondwana Beds of India</article-title><source> Acta Palaeobotanica</source><volume> 35</volume>,<fpage> 189</fpage>-<lpage>193</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.124411-ref37"><label>37</label><mixed-citation publication-type="other" xlink:type="simple">Joshi, A., Tewari, R., Agnihotri, D., Pillai, S.S.K. and Jain, R.K. (2015) Occurrence of Vertebraria indica (Unger) Feistmantel, 1877—an Evidence for Coal-Forming Vegetation in Kothagudem Area, Godavari Graben, Telangana. Current Science, 108, 330-333.</mixed-citation></ref><ref id="scirp.124411-ref38"><label>38</label><mixed-citation publication-type="other" xlink:type="simple">Maithy, P.K. (1965) Studies in the Glossopteris Flora of India 20. Noeggerathiopsis and Allied Remains from the Karharbari Beds, Giridih Coalfield, India. Journal of Palaeobotanist, 13, 94-100. https://doi.org/10.54991/jop.1964.684</mixed-citation></ref><ref id="scirp.124411-ref39"><label>39</label><mixed-citation publication-type="other" xlink:type="simple">Srivastava, A.K. and Tewari, R. (2002) Morphological and Cuticular Studies of Permain Noeggerathiopsis-Leaves. Geophytology, 32, 83-89.</mixed-citation></ref><ref id="scirp.124411-ref40"><label>40</label><mixed-citation publication-type="journal" xlink:type="simple"><name name-style="western"><surname>Lele</surname><given-names> K.M. </given-names></name>,<etal>et al</etal>. (<year>1976</year>)<article-title>Palaeoclimatic Implications of Gondwana Flora</article-title><source> Geophytology</source><volume> 6</volume>,<fpage> 207</fpage>-<lpage>229</lpage>.<pub-id pub-id-type="doi"></pub-id></mixed-citation></ref><ref id="scirp.124411-ref41"><label>41</label><mixed-citation publication-type="other" xlink:type="simple">Chandra, S. and Chandra, A. (1988) Vegetational Changes and Their Climatic Implications in Coal-Bearing Gondwana. Journal of Palaeosciences, 36, 74-86. https://doi.org/10.54991/jop.1987.1563</mixed-citation></ref><ref id="scirp.124411-ref42"><label>42</label><mixed-citation publication-type="other" xlink:type="simple">Joshi A. (2020) Dispersed Permian Megaspores from Rajmahal Basin, Jharkhand. Species, 21, 281-285.</mixed-citation></ref><ref id="scirp.124411-ref43"><label>43</label><mixed-citation publication-type="other" xlink:type="simple">Joshi, A. and Priya, R.K. (2021) First Report of Gangamopteris rajaensis from Rajmahal Gondwana Basin, Jharkhand, India. Geological Bulletin of Turkey, 64, 267-276.</mixed-citation></ref></ref-list></back></article>