EdenteV1, PascalFrancis, Curation, bibRecord, 000668

New evidence for Late Pleistocene human exploitation of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA

Identifieur interne : 000668 ( PascalFrancis/Curation ); précédent : 000667; suivant : 000669

New evidence for Late Pleistocene human exploitation of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA

Auteurs : Brian G. Redmond [États-Unis] ; H. Gregory Mcdonald [États-Unis] ; Haskel J. Greenfield [États-Unis] ; Matthew L. Burr [États-Unis]

Source :

World archaeology [ 0043-8243 ] ; 2012.

RBID : Pascal:13-0027756

Descripteurs français

Pascal (Inist)
- Pléistocène sup, Homme fossile, Prédation, Ostéologie, Taphonomie, Donnée MEB, C 14, Datation, Mammalia, Xenarthra, Biostratigraphie, Ossement, Megalonyx jeffersonii, Ohio.

English descriptors

KwdEn :
- C-14, Mammalia, Ohio, SEM data, Xenarthra, biostratigraphy, bones, dating, fossil man, osteology, predation, taphonomy, upper Pleistocene.

Abstract

The nature and extent of early human exploitation of late Pleistocene mega-mammals of North America have been vigorously debated; however, direct evidence of predation has been established for a small number of taxa. Until now, evidence of butchering and human utilization of ground sloths has been limited to South America. Osteological and taphonomic analyses of one curated collection of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA, have identified possible butchering marks on one femur. Historical research determined that the skeletal remains were originally recovered from a bog prior to 1915. Metric assessment of the ten skeletal elements identified this sloth as one of the largest individuals on record. SEM analysis of the left femur documented forty-one stone-tool marks, and their pattern and location indicate the filleting of leg muscles. XAD-purified bone collagen from the femur returned an AMS ¹⁴C radiocarbon age of 11,740±35 BP (13,738 to 13,435 cal. BP), which is as much as 700 years older than the calculated maximum age for Clovis. Although diminished somewhat by the lack of primary provenience data, these results offer significant evidence for late Pleistocene human exploitation of this North American taxon.

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A08	`01`	`1`	`ENG`	`@1 New evidence for Late Pleistocene human exploitation of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA`
A09	`01`	`1`	`ENG`	`@1 FAUNAL EXTINCTIONS AND INTRODUCTIONS`
A11	`01`	`1`		`@1 REDMOND (Brian G.)`
A11	`02`	`1`		`@1 MCDONALD (H. Gregory)`
A11	`03`	`1`		`@1 GREENFIELD (Haskel J.)`
A11	`04`	`1`		`@1 BURR (Matthew L.)`
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A14	`03`			`@1 Department of Anthropology, University of Manitoba @3 USA @Z 3 aut.`
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C01	`01`		`ENG`	@0 The nature and extent of early human exploitation of late Pleistocene mega-mammals of North America have been vigorously debated; however, direct evidence of predation has been established for a small number of taxa. Until now, evidence of butchering and human utilization of ground sloths has been limited to South America. Osteological and taphonomic analyses of one curated collection of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA, have identified possible butchering marks on one femur. Historical research determined that the skeletal remains were originally recovered from a bog prior to 1915. Metric assessment of the ten skeletal elements identified this sloth as one of the largest individuals on record. SEM analysis of the left femur documented forty-one stone-tool marks, and their pattern and location indicate the filleting of leg muscles. XAD-purified bone collagen from the femur returned an AMS ¹⁴C radiocarbon age of 11,740±35 BP (13,738 to 13,435 cal. BP), which is as much as 700 years older than the calculated maximum age for Clovis. Although diminished somewhat by the lack of primary provenience data, these results offer significant evidence for late Pleistocene human exploitation of this North American taxon.
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C03	`01`	`2`	`FRE`	`@0 Pléistocène sup @2 NX @5 01`
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C03	`02`	`2`	`FRE`	`@0 Homme fossile @5 02`
C03	`02`	`2`	`ENG`	`@0 fossil man @5 02`
C03	`02`	`2`	`SPA`	`@0 Hombre fósil @5 02`
C03	`03`	`2`	`FRE`	`@0 Prédation @5 03`
C03	`03`	`2`	`ENG`	`@0 predation @5 03`
C03	`03`	`2`	`SPA`	`@0 Rapiña @5 03`
C03	`04`	`2`	`FRE`	`@0 Ostéologie @5 04`
C03	`04`	`2`	`ENG`	`@0 osteology @5 04`
C03	`04`	`2`	`SPA`	`@0 Osteología @5 04`
C03	`05`	`2`	`FRE`	`@0 Taphonomie @5 05`
C03	`05`	`2`	`ENG`	`@0 taphonomy @5 05`
C03	`05`	`2`	`SPA`	`@0 Tafonomía @5 05`
C03	`06`	`2`	`FRE`	`@0 Donnée MEB @5 06`
C03	`06`	`2`	`ENG`	`@0 SEM data @5 06`
C03	`06`	`2`	`SPA`	`@0 Dato MEB @5 06`
C03	`07`	`2`	`FRE`	`@0 C 14 @5 07`
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C03	`08`	`2`	`ENG`	`@0 dating @5 08`
C03	`08`	`2`	`SPA`	`@0 Fechado @5 08`
C03	`09`	`2`	`FRE`	`@0 Mammalia @2 NY @5 10`
C03	`09`	`2`	`ENG`	`@0 Mammalia @2 NY @5 10`
C03	`09`	`2`	`SPA`	`@0 Mammalia @2 NY @5 10`
C03	`10`	`2`	`FRE`	`@0 Xenarthra @2 NY @5 11`
C03	`10`	`2`	`ENG`	`@0 Xenarthra @2 NY @5 11`
C03	`10`	`2`	`SPA`	`@0 Xenarthra @2 NY @5 11`
C03	`11`	`2`	`FRE`	`@0 Biostratigraphie @5 12`
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C03	`12`	`2`	`FRE`	`@0 Ossement @5 13`
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C03	`12`	`2`	`SPA`	`@0 Osamenta @5 13`
C03	`13`	`2`	`FRE`	`@0 Megalonyx jeffersonii @4 INC @5 52`
C03	`14`	`2`	`FRE`	`@0 Ohio @2 NG @5 61`
C03	`14`	`2`	`ENG`	`@0 Ohio @2 NG @5 61`
C03	`14`	`2`	`SPA`	`@0 Ohío @2 NG @5 61`
C07	`01`	`2`	`FRE`	`@0 Pléistocène @2 NX`
C07	`01`	`2`	`ENG`	`@0 Pleistocene @2 NX`
C07	`02`	`2`	`FRE`	`@0 Quaternaire @2 NX`
C07	`02`	`2`	`ENG`	`@0 Quaternary @2 NX`
C07	`02`	`2`	`SPA`	`@0 Cuaternario @2 NX`
C07	`03`	`2`	`FRE`	`@0 Cénozoïque @2 NX`
C07	`03`	`2`	`ENG`	`@0 Cenozoic @2 NX`
C07	`03`	`2`	`SPA`	`@0 Cenozoico @2 NX`
C07	`04`	`2`	`FRE`	`@0 Phanérozoïque @2 NX`
C07	`04`	`2`	`ENG`	`@0 Phanerozoic @2 NX`
C07	`04`	`2`	`SPA`	`@0 Fanerozoico @2 NX`
C07	`05`	`2`	`FRE`	`@0 Tetrapoda @2 NY`
C07	`05`	`2`	`ENG`	`@0 Tetrapoda @2 NY`
C07	`05`	`2`	`SPA`	`@0 Tetrapoda @2 NY`
C07	`06`	`2`	`FRE`	`@0 Vertebrata @2 NY`
C07	`06`	`2`	`ENG`	`@0 Vertebrata @2 NY`
C07	`06`	`2`	`SPA`	`@0 Vertebrata @2 NY`
C07	`07`	`2`	`FRE`	`@0 Chordata`
C07	`07`	`2`	`ENG`	`@0 Chordata`
C07	`07`	`2`	`SPA`	`@0 Chordata`
C07	`08`	`2`	`FRE`	`@0 Edentata @2 NY`
C07	`08`	`2`	`ENG`	`@0 Edentata @2 NY`
C07	`08`	`2`	`SPA`	`@0 Edentata @2 NY`
C07	`09`	`2`	`FRE`	`@0 Eutheria @2 NY`
C07	`09`	`2`	`ENG`	`@0 Eutheria @2 NY`
C07	`10`	`2`	`FRE`	`@0 Theria @2 NY`
C07	`10`	`2`	`ENG`	`@0 Theria @2 NY`
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C07	`12`	`2`	`ENG`	`@0 North America`
C07	`12`	`2`	`SPA`	`@0 America del norte`
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Pascal:13-0027756

Le document en format XML

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<front><div type="abstract" xml:lang="en">The nature and extent of early human exploitation of late Pleistocene mega-mammals of North America have been vigorously debated; however, direct evidence of predation has been established for a small number of taxa. Until now, evidence of butchering and human utilization of ground sloths has been limited to South America. Osteological and taphonomic analyses of one curated collection of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA, have identified possible butchering marks on one femur. Historical research determined that the skeletal remains were originally recovered from a bog prior to 1915. Metric assessment of the ten skeletal elements identified this sloth as one of the largest individuals on record. SEM analysis of the left femur documented forty-one stone-tool marks, and their pattern and location indicate the filleting of leg muscles. XAD-purified bone collagen from the femur returned an AMS <sup>14</sup>
C radiocarbon age of 11,740±35 BP (13,738 to 13,435 cal. BP), which is as much as 700 years older than the calculated maximum age for Clovis. Although diminished somewhat by the lack of primary provenience data, these results offer significant evidence for late Pleistocene human exploitation of this North American taxon.</div>
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<fA08 i1="01" i2="1" l="ENG"><s1>New evidence for Late Pleistocene human exploitation of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA</s1>
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<fA09 i1="01" i2="1" l="ENG"><s1>FAUNAL EXTINCTIONS AND INTRODUCTIONS</s1>
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<fA11 i1="01" i2="1"><s1>REDMOND (Brian G.)</s1>
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</fA11>
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<s9>limin.</s9>
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<s9>limin.</s9>
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<fA14 i1="01"><s1>Department of Archaeology, The Cleveland Museum of Natural History</s1>
<s3>USA</s3>
<sZ>1 aut.</sZ>
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<fA14 i1="02"><s1>Park Museum Management Program, National Park Service</s1>
<s2>Fort Collins, Colorado</s2>
<s3>USA</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Department of Anthropology, University of Manitoba</s1>
<s3>USA</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Firelands Historical Society</s1>
<s2>Norwalk, Ohio</s2>
<s3>USA</s3>
<sZ>4 aut.</sZ>
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<fA15 i1="01"><s1>University of Exeter</s1>
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<fC01 i1="01" l="ENG"><s0>The nature and extent of early human exploitation of late Pleistocene mega-mammals of North America have been vigorously debated; however, direct evidence of predation has been established for a small number of taxa. Until now, evidence of butchering and human utilization of ground sloths has been limited to South America. Osteological and taphonomic analyses of one curated collection of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA, have identified possible butchering marks on one femur. Historical research determined that the skeletal remains were originally recovered from a bog prior to 1915. Metric assessment of the ten skeletal elements identified this sloth as one of the largest individuals on record. SEM analysis of the left femur documented forty-one stone-tool marks, and their pattern and location indicate the filleting of leg muscles. XAD-purified bone collagen from the femur returned an AMS <sup>14</sup>
C radiocarbon age of 11,740±35 BP (13,738 to 13,435 cal. BP), which is as much as 700 years older than the calculated maximum age for Clovis. Although diminished somewhat by the lack of primary provenience data, these results offer significant evidence for late Pleistocene human exploitation of this North American taxon.</s0>
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<s5>01</s5>
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<s5>01</s5>
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<fC03 i1="02" i2="2" l="FRE"><s0>Homme fossile</s0>
<s5>02</s5>
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<fC03 i1="02" i2="2" l="ENG"><s0>fossil man</s0>
<s5>02</s5>
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<fC03 i1="02" i2="2" l="SPA"><s0>Hombre fósil</s0>
<s5>02</s5>
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<fC03 i1="03" i2="2" l="FRE"><s0>Prédation</s0>
<s5>03</s5>
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<fC03 i1="03" i2="2" l="ENG"><s0>predation</s0>
<s5>03</s5>
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<fC03 i1="03" i2="2" l="SPA"><s0>Rapiña</s0>
<s5>03</s5>
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<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>osteology</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Osteología</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Taphonomie</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>taphonomy</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Tafonomía</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Donnée MEB</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>SEM data</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Dato MEB</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>C 14</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>C-14</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>C 14</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Datation</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>dating</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Fechado</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Mammalia</s0>
<s2>NY</s2>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>Mammalia</s0>
<s2>NY</s2>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Mammalia</s0>
<s2>NY</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Xenarthra</s0>
<s2>NY</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Biostratigraphie</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>biostratigraphy</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Bioestratigrafía</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Ossement</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>bones</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Osamenta</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Megalonyx jeffersonii</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Ohio</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>Ohio</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Ohío</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Pléistocène</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Pleistocene</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Quaternaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Cuaternario</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Phanérozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Phanerozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Fanerozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="05" i2="2" l="SPA"><s0>Tetrapoda</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="06" i2="2" l="FRE"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="06" i2="2" l="SPA"><s0>Vertebrata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="07" i2="2" l="FRE"><s0>Chordata</s0>
</fC07>
<fC07 i1="07" i2="2" l="ENG"><s0>Chordata</s0>
</fC07>
<fC07 i1="07" i2="2" l="SPA"><s0>Chordata</s0>
</fC07>
<fC07 i1="08" i2="2" l="FRE"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="08" i2="2" l="ENG"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="08" i2="2" l="SPA"><s0>Edentata</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="09" i2="2" l="FRE"><s0>Eutheria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="09" i2="2" l="ENG"><s0>Eutheria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="10" i2="2" l="FRE"><s0>Theria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="10" i2="2" l="ENG"><s0>Theria</s0>
<s2>NY</s2>
</fC07>
<fC07 i1="11" i2="2" l="FRE"><s0>Etats Unis</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="11" i2="2" l="ENG"><s0>United States</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="11" i2="2" l="SPA"><s0>Estados Unidos</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="12" i2="2" l="FRE"><s0>Amérique du Nord</s0>
</fC07>
<fC07 i1="12" i2="2" l="ENG"><s0>North America</s0>
</fC07>
<fC07 i1="12" i2="2" l="SPA"><s0>America del norte</s0>
</fC07>
<fN21><s1>014</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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   |texte=   New evidence for Late Pleistocene human exploitation of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA
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New evidence for Late Pleistocene human exploitation of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA

New evidence for Late Pleistocene human exploitation of Jefferson's Ground Sloth (Megalonyx jeffersonii) from northern Ohio, USA

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