New geochronological, paleoclimatological, and archaeological data from the Narmada Valley hominin locality, central India
The oldest known fossil hominin in southern Asia was recovered from Hathnora in the Narmada Basin, central India in the early 1980's. Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at >236 ka, but not likely older than the early mi...
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description | The oldest known fossil hominin in southern Asia was recovered from Hathnora in the Narmada Basin, central India in the early 1980's. Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at >236
ka, but not likely older than the early middle Pleistocene. The calvaria, however, could be considerably younger. We report recent fieldwork at Hathnora and associated Quaternary type-sections that has provided new geological and archaeological insights. The portion of the exposed ‘Boulder Conglomerate’ within the Surajkund Formation, which forms a relict terrace and has yielded the hominin fossils, contains reworked and stylistically mixed lithic artifacts and temporally mixed fauna. Three mammalian teeth stratigraphically associated with the hominin calvaria were dated by standard electron spin resonance (ESR). Assuming an early uranium uptake (EU) model for the teeth, two samples collected from the reworked surface deposit averaged 49
±
1
ka (83
±
2
ka, assuming linear uptake [LU]; 196
±
7
ka assuming recent uptake [RU]). Another sample recovered from freshly exposed, crossbedded gravels averaged 93
±
5
ka (EU), 162
±
8
ka (LU) or 407
±
21
ka (RU). While linear uptake models usually provide the most accurate ages for this environment and time range, the EU ages represent the minimum possible age for fossils in the deposit. Regardless, the fossils are clearly reworked and temporally mixed. Therefore, the current data constrains the minimum possible age for the calvaria to 49
±
1
ka, although it could have been reworked and deposited into the Hathnora deposit any time after 160
ka (given the LU uptake ages) or earlier (given the RU ages). At Hathnora, carbonaceous clay, bivalve shells, and a bovid tooth recovered from layers belonging to the overlying Baneta Formation have yielded
14C ages of 35.66
±
2.54
cal ky BP, 24.28
±
0.39
cal ky BP, and 13.15
±
0.34
ky BP, respectively. Additional surveys yielded numerous lithics and fossils on the surface and within the stratigraphic sequence. At the foot of the Vindhyan Hills 2
km from the river, we recovered a typologically Early Acheulean assemblage comprised of asymmetrical bifaces, large cleavers with minimal working, trihedral picks, and flake tools in fresh condition. These tools may be the oldest Acheulean in the Narmada Valley. Several lithics recovered from the Dhansi Formation may represent the first unequivocal evidence for an early Pleistocene hominin pres |
doi_str_mv | 10.1016/j.jhevol.2008.08.023 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_66858034</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0047248408001978</els_id><sourcerecordid>66858034</sourcerecordid><originalsourceid>FETCH-LOGICAL-c421t-2df7d7077465222698cc4579f0cfcc66c07358aff20119d69a932e30c9fa5fae3</originalsourceid><addsrcrecordid>eNqFkU-LFDEQxYMo7rj6DURy0dP2mKTTSfdFWBb_LCzrRb2GMqlsZ0h3xqRnZfz0ZpjRvSkUFDx-ryjeI-QlZ2vOuHq7WW9GvE9xLRjr14cR7SOy4mzoml4x9ZisGJO6EbKXZ-RZKRvG2CBb8ZSc8YHzvld6RX7d4k96h8mOOc0pprtgIV7QLcSqxTDB8iDC7ChkOwL-0aiDBajPaaLLiPQW8gQO6DeIEfd0TFOYw0xjqmhY9hfU4rzkarueXYDn5ImHWPDFaZ-Trx_ef7n61Nx8_nh9dXnTWCn40gjntdNMa6k6IYQaemtlpwfPrLdWKct02_XgvWCcD04NMLQCW2YHD50HbM_Jm-PdbU4_dlgWM4ViMUaYMe2KUarvetbK_4Kt5rImqisoj6DNqZSM3mxzjSrvDWfmUI7ZmGM55lCOOYxoq-3V6f7u-4TuwXRqowKvTwCUGpnPMNtQ_nKCc6nqE5V7d-SwxnYfMJtiA84WXchoF-NS-PcnvwFWN7CG</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>37140477</pqid></control><display><type>article</type><title>New geochronological, paleoclimatological, and archaeological data from the Narmada Valley hominin locality, central India</title><source>MEDLINE</source><source>Access via ScienceDirect (Elsevier)</source><creator>Patnaik, Rajeev ; Chauhan, Parth R. ; Rao, M.R. ; Blackwell, B.A.B. ; Skinner, A.R. ; Sahni, Ashok ; Chauhan, M.S. ; Khan, H.S.</creator><creatorcontrib>Patnaik, Rajeev ; Chauhan, Parth R. ; Rao, M.R. ; Blackwell, B.A.B. ; Skinner, A.R. ; Sahni, Ashok ; Chauhan, M.S. ; Khan, H.S.</creatorcontrib><description>The oldest known fossil hominin in southern Asia was recovered from Hathnora in the Narmada Basin, central India in the early 1980's. Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at >236
ka, but not likely older than the early middle Pleistocene. The calvaria, however, could be considerably younger. We report recent fieldwork at Hathnora and associated Quaternary type-sections that has provided new geological and archaeological insights. The portion of the exposed ‘Boulder Conglomerate’ within the Surajkund Formation, which forms a relict terrace and has yielded the hominin fossils, contains reworked and stylistically mixed lithic artifacts and temporally mixed fauna. Three mammalian teeth stratigraphically associated with the hominin calvaria were dated by standard electron spin resonance (ESR). Assuming an early uranium uptake (EU) model for the teeth, two samples collected from the reworked surface deposit averaged 49
±
1
ka (83
±
2
ka, assuming linear uptake [LU]; 196
±
7
ka assuming recent uptake [RU]). Another sample recovered from freshly exposed, crossbedded gravels averaged 93
±
5
ka (EU), 162
±
8
ka (LU) or 407
±
21
ka (RU). While linear uptake models usually provide the most accurate ages for this environment and time range, the EU ages represent the minimum possible age for fossils in the deposit. Regardless, the fossils are clearly reworked and temporally mixed. Therefore, the current data constrains the minimum possible age for the calvaria to 49
±
1
ka, although it could have been reworked and deposited into the Hathnora deposit any time after 160
ka (given the LU uptake ages) or earlier (given the RU ages). At Hathnora, carbonaceous clay, bivalve shells, and a bovid tooth recovered from layers belonging to the overlying Baneta Formation have yielded
14C ages of 35.66
±
2.54
cal ky BP, 24.28
±
0.39
cal ky BP, and 13.15
±
0.34
ky BP, respectively. Additional surveys yielded numerous lithics and fossils on the surface and within the stratigraphic sequence. At the foot of the Vindhyan Hills 2
km from the river, we recovered a typologically Early Acheulean assemblage comprised of asymmetrical bifaces, large cleavers with minimal working, trihedral picks, and flake tools in fresh condition. These tools may be the oldest Acheulean in the Narmada Valley. Several lithics recovered from the Dhansi Formation may represent the first unequivocal evidence for an early Pleistocene hominin presence in India. In situ invertebrate and vertebrate fossils, pollen, and spores indicate a warm, humid climate during the late middle Pleistocene. High uranium concentrations in the mammalian teeth indicate exposure to saline water, suggesting highly evaporative conditions in the past. Late Pleistocene sediment dated between 24.28
±
0.39
cal ky BP and 13.15
±
340
ky BP has yielded pollen and spores indicating cool, dry climatic conditions corresponding to Oxygen Isotope Stage 2 (OIS 2). An early Holocene palynological assemblage from the type locality at Baneta shows evidence for relatively dry conditions and a deciduous forest within the region. The Dhansi Formation provisionally replaces the Pilikarar Formation as the oldest Quaternary formation within the central Narmada Basin. The Baneta Formation, previously dated at 70
ka to 128
ka, correlates with the late Pleistocene and early Holocene. Our results highlight the need for further Quaternary geological and paleoanthropological research within the Narmada Basin, especially because dam construction threatens these deposits.</description><identifier>ISSN: 0047-2484</identifier><identifier>EISSN: 1095-8606</identifier><identifier>DOI: 10.1016/j.jhevol.2008.08.023</identifier><identifier>PMID: 19118867</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>Animals ; Archaeology ; Asia ; Biological Evolution ; Climate ; Fossil hominin site ; Fossils ; Geochronology ; Geology ; History, Ancient ; Hominidae ; Hominids ; Human paleontology ; Humans ; India ; Lithics ; Methodology and general studies ; Middle East and Indian Peninsula ; Palaeolithic and mesolithic ; Paleoanthropology ; Paleoclimatology ; Paleodontology ; Paleontology ; Pleistocene ; Prehistoric archaeology ; Prehistory ; Prehistory and protohistory ; Quaternary stratigraphy ; Skull</subject><ispartof>Journal of human evolution, 2009-02, Vol.56 (2), p.114-133</ispartof><rights>2008 Elsevier Ltd</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c421t-2df7d7077465222698cc4579f0cfcc66c07358aff20119d69a932e30c9fa5fae3</citedby><cites>FETCH-LOGICAL-c421t-2df7d7077465222698cc4579f0cfcc66c07358aff20119d69a932e30c9fa5fae3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.jhevol.2008.08.023$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>315,782,786,3554,27933,27934,46004</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=21146371$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/19118867$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Patnaik, Rajeev</creatorcontrib><creatorcontrib>Chauhan, Parth R.</creatorcontrib><creatorcontrib>Rao, M.R.</creatorcontrib><creatorcontrib>Blackwell, B.A.B.</creatorcontrib><creatorcontrib>Skinner, A.R.</creatorcontrib><creatorcontrib>Sahni, Ashok</creatorcontrib><creatorcontrib>Chauhan, M.S.</creatorcontrib><creatorcontrib>Khan, H.S.</creatorcontrib><title>New geochronological, paleoclimatological, and archaeological data from the Narmada Valley hominin locality, central India</title><title>Journal of human evolution</title><addtitle>J Hum Evol</addtitle><description>The oldest known fossil hominin in southern Asia was recovered from Hathnora in the Narmada Basin, central India in the early 1980's. Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at >236
ka, but not likely older than the early middle Pleistocene. The calvaria, however, could be considerably younger. We report recent fieldwork at Hathnora and associated Quaternary type-sections that has provided new geological and archaeological insights. The portion of the exposed ‘Boulder Conglomerate’ within the Surajkund Formation, which forms a relict terrace and has yielded the hominin fossils, contains reworked and stylistically mixed lithic artifacts and temporally mixed fauna. Three mammalian teeth stratigraphically associated with the hominin calvaria were dated by standard electron spin resonance (ESR). Assuming an early uranium uptake (EU) model for the teeth, two samples collected from the reworked surface deposit averaged 49
±
1
ka (83
±
2
ka, assuming linear uptake [LU]; 196
±
7
ka assuming recent uptake [RU]). Another sample recovered from freshly exposed, crossbedded gravels averaged 93
±
5
ka (EU), 162
±
8
ka (LU) or 407
±
21
ka (RU). While linear uptake models usually provide the most accurate ages for this environment and time range, the EU ages represent the minimum possible age for fossils in the deposit. Regardless, the fossils are clearly reworked and temporally mixed. Therefore, the current data constrains the minimum possible age for the calvaria to 49
±
1
ka, although it could have been reworked and deposited into the Hathnora deposit any time after 160
ka (given the LU uptake ages) or earlier (given the RU ages). At Hathnora, carbonaceous clay, bivalve shells, and a bovid tooth recovered from layers belonging to the overlying Baneta Formation have yielded
14C ages of 35.66
±
2.54
cal ky BP, 24.28
±
0.39
cal ky BP, and 13.15
±
0.34
ky BP, respectively. Additional surveys yielded numerous lithics and fossils on the surface and within the stratigraphic sequence. At the foot of the Vindhyan Hills 2
km from the river, we recovered a typologically Early Acheulean assemblage comprised of asymmetrical bifaces, large cleavers with minimal working, trihedral picks, and flake tools in fresh condition. These tools may be the oldest Acheulean in the Narmada Valley. Several lithics recovered from the Dhansi Formation may represent the first unequivocal evidence for an early Pleistocene hominin presence in India. In situ invertebrate and vertebrate fossils, pollen, and spores indicate a warm, humid climate during the late middle Pleistocene. High uranium concentrations in the mammalian teeth indicate exposure to saline water, suggesting highly evaporative conditions in the past. Late Pleistocene sediment dated between 24.28
±
0.39
cal ky BP and 13.15
±
340
ky BP has yielded pollen and spores indicating cool, dry climatic conditions corresponding to Oxygen Isotope Stage 2 (OIS 2). An early Holocene palynological assemblage from the type locality at Baneta shows evidence for relatively dry conditions and a deciduous forest within the region. The Dhansi Formation provisionally replaces the Pilikarar Formation as the oldest Quaternary formation within the central Narmada Basin. The Baneta Formation, previously dated at 70
ka to 128
ka, correlates with the late Pleistocene and early Holocene. Our results highlight the need for further Quaternary geological and paleoanthropological research within the Narmada Basin, especially because dam construction threatens these deposits.</description><subject>Animals</subject><subject>Archaeology</subject><subject>Asia</subject><subject>Biological Evolution</subject><subject>Climate</subject><subject>Fossil hominin site</subject><subject>Fossils</subject><subject>Geochronology</subject><subject>Geology</subject><subject>History, Ancient</subject><subject>Hominidae</subject><subject>Hominids</subject><subject>Human paleontology</subject><subject>Humans</subject><subject>India</subject><subject>Lithics</subject><subject>Methodology and general studies</subject><subject>Middle East and Indian Peninsula</subject><subject>Palaeolithic and mesolithic</subject><subject>Paleoanthropology</subject><subject>Paleoclimatology</subject><subject>Paleodontology</subject><subject>Paleontology</subject><subject>Pleistocene</subject><subject>Prehistoric archaeology</subject><subject>Prehistory</subject><subject>Prehistory and protohistory</subject><subject>Quaternary stratigraphy</subject><subject>Skull</subject><issn>0047-2484</issn><issn>1095-8606</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><recordid>eNqFkU-LFDEQxYMo7rj6DURy0dP2mKTTSfdFWBb_LCzrRb2GMqlsZ0h3xqRnZfz0ZpjRvSkUFDx-ryjeI-QlZ2vOuHq7WW9GvE9xLRjr14cR7SOy4mzoml4x9ZisGJO6EbKXZ-RZKRvG2CBb8ZSc8YHzvld6RX7d4k96h8mOOc0pprtgIV7QLcSqxTDB8iDC7ChkOwL-0aiDBajPaaLLiPQW8gQO6DeIEfd0TFOYw0xjqmhY9hfU4rzkarueXYDn5ImHWPDFaZ-Trx_ef7n61Nx8_nh9dXnTWCn40gjntdNMa6k6IYQaemtlpwfPrLdWKct02_XgvWCcD04NMLQCW2YHD50HbM_Jm-PdbU4_dlgWM4ViMUaYMe2KUarvetbK_4Kt5rImqisoj6DNqZSM3mxzjSrvDWfmUI7ZmGM55lCOOYxoq-3V6f7u-4TuwXRqowKvTwCUGpnPMNtQ_nKCc6nqE5V7d-SwxnYfMJtiA84WXchoF-NS-PcnvwFWN7CG</recordid><startdate>20090201</startdate><enddate>20090201</enddate><creator>Patnaik, Rajeev</creator><creator>Chauhan, Parth R.</creator><creator>Rao, M.R.</creator><creator>Blackwell, B.A.B.</creator><creator>Skinner, A.R.</creator><creator>Sahni, Ashok</creator><creator>Chauhan, M.S.</creator><creator>Khan, H.S.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8BJ</scope><scope>FQK</scope><scope>JBE</scope><scope>7X8</scope></search><sort><creationdate>20090201</creationdate><title>New geochronological, paleoclimatological, and archaeological data from the Narmada Valley hominin locality, central India</title><author>Patnaik, Rajeev ; Chauhan, Parth R. ; Rao, M.R. ; Blackwell, B.A.B. ; Skinner, A.R. ; Sahni, Ashok ; Chauhan, M.S. ; Khan, H.S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c421t-2df7d7077465222698cc4579f0cfcc66c07358aff20119d69a932e30c9fa5fae3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Animals</topic><topic>Archaeology</topic><topic>Asia</topic><topic>Biological Evolution</topic><topic>Climate</topic><topic>Fossil hominin site</topic><topic>Fossils</topic><topic>Geochronology</topic><topic>Geology</topic><topic>History, Ancient</topic><topic>Hominidae</topic><topic>Hominids</topic><topic>Human paleontology</topic><topic>Humans</topic><topic>India</topic><topic>Lithics</topic><topic>Methodology and general studies</topic><topic>Middle East and Indian Peninsula</topic><topic>Palaeolithic and mesolithic</topic><topic>Paleoanthropology</topic><topic>Paleoclimatology</topic><topic>Paleodontology</topic><topic>Paleontology</topic><topic>Pleistocene</topic><topic>Prehistoric archaeology</topic><topic>Prehistory</topic><topic>Prehistory and protohistory</topic><topic>Quaternary stratigraphy</topic><topic>Skull</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Patnaik, Rajeev</creatorcontrib><creatorcontrib>Chauhan, Parth R.</creatorcontrib><creatorcontrib>Rao, M.R.</creatorcontrib><creatorcontrib>Blackwell, B.A.B.</creatorcontrib><creatorcontrib>Skinner, A.R.</creatorcontrib><creatorcontrib>Sahni, Ashok</creatorcontrib><creatorcontrib>Chauhan, M.S.</creatorcontrib><creatorcontrib>Khan, H.S.</creatorcontrib><collection>Pascal-Francis</collection><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>International Bibliography of the Social Sciences (IBSS)</collection><collection>International Bibliography of the Social Sciences</collection><collection>International Bibliography of the Social Sciences</collection><collection>MEDLINE - Academic</collection><jtitle>Journal of human evolution</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Patnaik, Rajeev</au><au>Chauhan, Parth R.</au><au>Rao, M.R.</au><au>Blackwell, B.A.B.</au><au>Skinner, A.R.</au><au>Sahni, Ashok</au><au>Chauhan, M.S.</au><au>Khan, H.S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>New geochronological, paleoclimatological, and archaeological data from the Narmada Valley hominin locality, central India</atitle><jtitle>Journal of human evolution</jtitle><addtitle>J Hum Evol</addtitle><date>2009-02-01</date><risdate>2009</risdate><volume>56</volume><issue>2</issue><spage>114</spage><epage>133</epage><pages>114-133</pages><issn>0047-2484</issn><eissn>1095-8606</eissn><abstract>The oldest known fossil hominin in southern Asia was recovered from Hathnora in the Narmada Basin, central India in the early 1980's. Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at >236
ka, but not likely older than the early middle Pleistocene. The calvaria, however, could be considerably younger. We report recent fieldwork at Hathnora and associated Quaternary type-sections that has provided new geological and archaeological insights. The portion of the exposed ‘Boulder Conglomerate’ within the Surajkund Formation, which forms a relict terrace and has yielded the hominin fossils, contains reworked and stylistically mixed lithic artifacts and temporally mixed fauna. Three mammalian teeth stratigraphically associated with the hominin calvaria were dated by standard electron spin resonance (ESR). Assuming an early uranium uptake (EU) model for the teeth, two samples collected from the reworked surface deposit averaged 49
±
1
ka (83
±
2
ka, assuming linear uptake [LU]; 196
±
7
ka assuming recent uptake [RU]). Another sample recovered from freshly exposed, crossbedded gravels averaged 93
±
5
ka (EU), 162
±
8
ka (LU) or 407
±
21
ka (RU). While linear uptake models usually provide the most accurate ages for this environment and time range, the EU ages represent the minimum possible age for fossils in the deposit. Regardless, the fossils are clearly reworked and temporally mixed. Therefore, the current data constrains the minimum possible age for the calvaria to 49
±
1
ka, although it could have been reworked and deposited into the Hathnora deposit any time after 160
ka (given the LU uptake ages) or earlier (given the RU ages). At Hathnora, carbonaceous clay, bivalve shells, and a bovid tooth recovered from layers belonging to the overlying Baneta Formation have yielded
14C ages of 35.66
±
2.54
cal ky BP, 24.28
±
0.39
cal ky BP, and 13.15
±
0.34
ky BP, respectively. Additional surveys yielded numerous lithics and fossils on the surface and within the stratigraphic sequence. At the foot of the Vindhyan Hills 2
km from the river, we recovered a typologically Early Acheulean assemblage comprised of asymmetrical bifaces, large cleavers with minimal working, trihedral picks, and flake tools in fresh condition. These tools may be the oldest Acheulean in the Narmada Valley. Several lithics recovered from the Dhansi Formation may represent the first unequivocal evidence for an early Pleistocene hominin presence in India. In situ invertebrate and vertebrate fossils, pollen, and spores indicate a warm, humid climate during the late middle Pleistocene. High uranium concentrations in the mammalian teeth indicate exposure to saline water, suggesting highly evaporative conditions in the past. Late Pleistocene sediment dated between 24.28
±
0.39
cal ky BP and 13.15
±
340
ky BP has yielded pollen and spores indicating cool, dry climatic conditions corresponding to Oxygen Isotope Stage 2 (OIS 2). An early Holocene palynological assemblage from the type locality at Baneta shows evidence for relatively dry conditions and a deciduous forest within the region. The Dhansi Formation provisionally replaces the Pilikarar Formation as the oldest Quaternary formation within the central Narmada Basin. The Baneta Formation, previously dated at 70
ka to 128
ka, correlates with the late Pleistocene and early Holocene. Our results highlight the need for further Quaternary geological and paleoanthropological research within the Narmada Basin, especially because dam construction threatens these deposits.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><pmid>19118867</pmid><doi>10.1016/j.jhevol.2008.08.023</doi><tpages>20</tpages></addata></record> |
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subjects | Animals Archaeology Asia Biological Evolution Climate Fossil hominin site Fossils Geochronology Geology History, Ancient Hominidae Hominids Human paleontology Humans India Lithics Methodology and general studies Middle East and Indian Peninsula Palaeolithic and mesolithic Paleoanthropology Paleoclimatology Paleodontology Paleontology Pleistocene Prehistoric archaeology Prehistory Prehistory and protohistory Quaternary stratigraphy Skull |
title | New geochronological, paleoclimatological, and archaeological data from the Narmada Valley hominin locality, central India |
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