<?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">OJG</journal-id><journal-title-group><journal-title>Open Journal of Geology</journal-title></journal-title-group><issn pub-type="epub">2161-7570</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ojg.2019.910050</article-id><article-id pub-id-type="publisher-id">OJG-95231</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>
 
 
  The Origin and Diversification of Plant Family Dipterocarpaceae
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mahi</surname><given-names>Bansal</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Shivaprakash</surname><given-names>K. Nagaraju</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vandana</surname><given-names>Prasad</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff2"><addr-line>Centre for Structural and Functional Genomics, Biology Department, Concordia University, Montreal, Canada</addr-line></aff><aff id="aff1"><addr-line>Terminal Cretaceous-Cenozoic Ecosystem Laboratory, Birbal Sahni Institute of Palaeosciences, Lucknow, India</addr-line></aff><pub-date pub-type="epub"><day>20</day><month>09</month><year>2019</year></pub-date><volume>09</volume><issue>10</issue><fpage>593</fpage><lpage>596</lpage><history><date date-type="received"><day>15,</day>	<month>August</month>	<year>2019</year></date><date date-type="rev-recd"><day>20,</day>	<month>September</month>	<year>2019</year>	</date><date date-type="accepted"><day>23,</day>	<month>September</month>	<year>2019</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 Dipterocarpaceae plant family, that shows a disjunct distribution in Gondwanan continents and Southeast Asia, is a dominant constituent of the tropical rain forests of Southeast Asia. The high species diversity of Dipterocarpaceae in SE Asian rain forests suggests its origin from SE Asia. However, its fossil history is much younger, from Oligocene, from the region. Based on the pollen fossil records from the late Cretaceous-early Paleogene sedimentary sequences of Indian subcontinent and the contemporaneous distribution of its extant taxa, evolutionary history of Dipterocarpaceae has been traced. The study suggests a West Gondwanan origin for this family. Present study also provides first evidence of Dipterocarpaceae genus 
  <em>Vateriopsis</em> (endemic in Seychelles) type fossil pollen record from the late Cretaceous and early Palaeogene sedimentary sequences of western Indian margin.
 
</p></abstract><kwd-group><kwd>Fossil</kwd><kwd> &lt;i&gt;Vateriospis&lt;/i&gt;</kwd><kwd> Pollen</kwd><kwd> Cretaceous</kwd><kwd> Dipterocarpaceae</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Dipterocarpaceae, an economically important arborescent family distributed in SE Asian tropical regions, is important for the production of timber, camphor and resins. There exist a lot of opinions about its systematic classification [<xref ref-type="bibr" rid="scirp.95231-ref1">1</xref>] . The family is subdivided into three subfamilies: 1) Monotoideae, restricted to Africa, Madagascar and South America; 2) Pakaraimoideae, endemic to South America; 3) Dipterocarpoideae, distributed in SE Asia [<xref ref-type="bibr" rid="scirp.95231-ref2">2</xref>] . Except the two genera, Pseudomonotes and Marquesia, the representatives of Monotoideae distributed across Africa and Madagascar cultivate in seasonally dry forests. Whereas members of Pakaraimoideae and Dipterocarpoideae subfamilies prefer lowland rain forest. It has been found that various species of Dipterocarpoideae have the adaptability to seasonally wet and aseasonal perhumid tropical regions of SE Asia [<xref ref-type="bibr" rid="scirp.95231-ref1">1</xref>] . Due to more plasticity in the climatic adaptive nature, members of Dipterocarpoideae exhibit greater species diversity compared to the other two subfamilies. The family is disseminated across continents following a strict disjunct distribution pattern which raises a question of its place and time of origin. Dipterocarpoideae clade dominates in SE Asia and almost 80% of its diversity has been found to occur in wet forest of SE Asia particularly in Western Malaysia (Borneo), and hence SE Asia was considered to be its centre of origin [<xref ref-type="bibr" rid="scirp.95231-ref3">3</xref>] . There are two plausible hypotheses proposed for the evolutionary history and biogeography of the family Dipterocarpaceae. One hypothesis supports a SE Asian origin (Into India hypothesis). The other suggests a Gondwanan origin (Out of India hypothesis) [<xref ref-type="bibr" rid="scirp.95231-ref3">3</xref>] . In the present study, we are trying to assess both biogeographic hypotheses based on fossil data.</p></sec><sec id="s2"><title>2. Material and Method</title><p>Studied samples were collected from three sites: 1) Late Cretaceous infratrappean bore core samples from Yeotmal region, Maharashtra; 2) Late Cretaceous intertrappean samples from Gowmukh area, Madhya Pradesh; 3) Early Palaeogene (Danian) samples from Gurha lignite mine, Bikaner region, Rajasthan. For comparison purposes, extant flower buds of Vateriopsis collected from Seychelles were acetolysed for pollen study and the extant pollen were compared with the fossil palynomorphs.</p></sec><sec id="s3"><title>3. Results</title><p>The current study finds the presence of Vateriopsis type pollen fossil from the Upper Cretaceaous and Lower Palaeogene deposits of intertrappeans of central India and Bikaner Basin, Rajasthan, India, respectively. This study also documents the variety of Dipterocarpus type pollen fossils from the Upper Cretaceous of infratrappeans and intertrappeans of Maharashtra and Madhya Pradesh, central India, and the Lower Paleogene of Bikaner Basin, Rajasthan, western India.</p></sec><sec id="s4"><title>4. Discussion and Conclusion</title><p>The Late Cretaceous Vateriopsis and Dipterocarpus type fossil pollen records suggest the Out of India hypothesis. Dipterocarpus type fossil pollen is recovered from the Indian Upper Cretaceous, the time when Indo-Seychelles plate was in surficial contact with Africa [<xref ref-type="bibr" rid="scirp.95231-ref4">4</xref>] . The distance between Asia and India during the Late Cretaceous was too large and could not facilitate the dispersal of the family. The presence of Vateriopsis type fossil pollen in Indian Lower Paleogene is the time just before the separation of Indo-Greater Somalaria from Seychelles [<xref ref-type="bibr" rid="scirp.95231-ref4">4</xref>] . The present distribution of Vateriopsis in Seychelles suggests its migration from India. Moreover, the presence of possible Dipterocarpus fossils from Africa [<xref ref-type="bibr" rid="scirp.95231-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.95231-ref5">5</xref>] , a continent where only Monotes is found in the present day, also strongly indicates the diversification of the family on Gondwanan landmass. Our consent of Out of India hypothesis for Dipterocarpaceae dispersal in SE Asia is much more strengthened by the presence of polycadinene resin in the Upper Eocene of Mayanmar which was a part of Indian plate before its collision to Asia [<xref ref-type="bibr" rid="scirp.95231-ref6">6</xref>] . This suggests that the family might have migrated to Asia after the contact between India and Asia was established.</p><p>Furthermore the sharing of ectomycorrhizal symbiotic relation between Dipterocarpaceae and Sarcolaenaceae, a family endemic to Madagascar in present time, signifies that both families share a common ancestor [<xref ref-type="bibr" rid="scirp.95231-ref7">7</xref>] . The previously stated fact and the only Miocene fossil record of Sarcolaenaceae from Africa [<xref ref-type="bibr" rid="scirp.95231-ref8">8</xref>] imply that the diversification of the families should have occurred on the Gondwana landmass before the separation of Madagascar from India-Seychelles block.</p></sec><sec id="s5"><title>Acknowledgements</title><p>The study is supported by the project MoES/P.O.(GeoSci.)/36/2014. This is a contribution to UNESCO-IUGS IGCP Project 679.</p></sec><sec id="s6"><title>Conflicts of Interest</title><p>The authors declare no conflicts of interest regarding the publication of this paper.</p></sec><sec id="s7"><title>Cite this paper</title><p>Bansal, M., Nagaraju, S.K. and Prasad, V. (2019) The Origin and Diversification of Plant Family Dipterocarpaceae. 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