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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Veröffentlicht in:Journal of human evolution 2009-02, Vol.56 (2), p.114-133
Hauptverfasser: Patnaik, Rajeev, Chauhan, Parth R., Rao, M.R., Blackwell, B.A.B., Skinner, A.R., Sahni, Ashok, Chauhan, M.S., Khan, H.S.
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container_end_page 133
container_issue 2
container_start_page 114
container_title Journal of human evolution
container_volume 56
creator Patnaik, Rajeev
Chauhan, Parth R.
Rao, M.R.
Blackwell, B.A.B.
Skinner, A.R.
Sahni, Ashok
Chauhan, M.S.
Khan, H.S.
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
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Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at &gt;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. 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Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at &gt;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. 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Its age and taxonomic affinities, however, have remained uncertain. Current estimates place its maximum age at &gt;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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source MEDLINE; Access via ScienceDirect (Elsevier)
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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