Homo floresiensis-like fossils from the early Middle Pleistocene of Flores
Abstract
The evolutionary origin of Homo floresiensis,
a diminutive hominin species previously known only by skeletal remains
from Liang Bua in western Flores, Indonesia, has been intensively
debated. It is a matter of controversy whether this primitive form,
dated to the Late Pleistocene, evolved from early Asian Homo erectus and represents a unique and striking case of evolutionary reversal in hominin body and brain size within an insular environment1,2,3,4.
The alternative hypothesis is that H. floresiensis derived from an older, smaller-brained member of our genus, such as Homo habilis, or perhaps even late Australopithecus, signalling a hitherto undocumented dispersal of hominins from Africa into eastern Asia by two million years ago (2 Ma)5,6. Here we describe hominin fossils excavated in 2014 from an early Middle Pleistocene site (Mata Menge) in the So’a Basin of central Flores.
These specimens comprise a mandible fragment and six isolated teeth belonging to at least three small-jawed and small-toothed individuals. Dating to ~0.7 Ma, these fossils now constitute the oldest hominin remains from Flores7.
The Mata Menge mandible and teeth are similar in dimensions and morphological characteristics to those of H. floresiensis from Liang Bua. The exception is the mandibular first molar, which retains a more primitive condition.
Notably, the Mata Menge mandible and molar are even smaller in size than those of the two existing H. floresiensis individuals from Liang Bua. The Mata Menge fossils are derived compared with Australopithecus and H. habilis, and so tend to support the view that H. floresiensis is a dwarfed descendent of early Asian H. erectus. Our findings suggest that hominins on Flores had acquired extremely small body size and other morphological traits specific to H. floresiensis at an unexpectedly early time.
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The alternative hypothesis is that H. floresiensis derived from an older, smaller-brained member of our genus, such as Homo habilis, or perhaps even late Australopithecus, signalling a hitherto undocumented dispersal of hominins from Africa into eastern Asia by two million years ago (2 Ma)5,6. Here we describe hominin fossils excavated in 2014 from an early Middle Pleistocene site (Mata Menge) in the So’a Basin of central Flores.
These specimens comprise a mandible fragment and six isolated teeth belonging to at least three small-jawed and small-toothed individuals. Dating to ~0.7 Ma, these fossils now constitute the oldest hominin remains from Flores7.
The Mata Menge mandible and teeth are similar in dimensions and morphological characteristics to those of H. floresiensis from Liang Bua. The exception is the mandibular first molar, which retains a more primitive condition.
Notably, the Mata Menge mandible and molar are even smaller in size than those of the two existing H. floresiensis individuals from Liang Bua. The Mata Menge fossils are derived compared with Australopithecus and H. habilis, and so tend to support the view that H. floresiensis is a dwarfed descendent of early Asian H. erectus. Our findings suggest that hominins on Flores had acquired extremely small body size and other morphological traits specific to H. floresiensis at an unexpectedly early time.
References
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Acknowledgements
The So’a Basin project was funded by an Australian Research Council (ARC) Discovery
grant (DP1093342) awarded to M.J.M. and A.B., and directed by M.J.M.
(2010–2013) and G.v.d.B. (2013–2015). The Geological Survey Institute
(GSI) of Bandung, Indonesia, provided additional financial and technical
support. G.v.d.B.’s research was also supported by ARC Future
Fellowship FT100100384. M.W.M. was funded by ARC grant DP1096558.
Quadlab is funded by a grant to M.S. from the Villum Foundation. M.D.
received funding from a Marie Curie International Outgoing Fellowship of
the EU’s Seventh Framework Programme (FP7/2007-2013), awarded under REA
Grant Agreement No. PIOF-GA-2013-626474. B.V.A. received funding from a
Victoria University of Wellington Science Faculty Research Grant
(201255). For permission to undertake this research, we thank the
Indonesian State Ministry of Research and Technology (RISTEK), the
former Heads of the Geological Agency (R. Sukyiar and Surono), the
successive directors of the GSI (S. Permanandewi, Y. Kusumahbrata
(formerly) and A. Pribadi) and Bandung’s Geology Museum (S. Baskoro and
O. Abdurahman). Local research permissions were issued by the provincial
government of East Nusa Tenggara at Kupang, and the Ngada and Nage Keo
administrations. We also thank the Ngada Tourism and Culture and
Education Departments for their ongoing support. In addition, we
acknowledge support and advice provided by I. Setiadi, D. Pribadi, and
Suyono (GSI), the Pusat Penelitian Arkeologi Nasional (ARKENAS) in
Jakarta, and J. T. Solo of the provincial Culture and Tourism office in
Kupang. Scientific and technical personnel involved in the fieldwork
included: T. Suryana, S. Sonjaya, H. Oktariana, I. Sutisna, A. Rahman,
S. Bronto, E. Sukandar, A. Gunawan, Widji, A. T. Hascaryo, Jatmiko, S.
Wasisto, R. A. Due, S. Hayes, Y. Perston, B. Pillans, K. Grant, M.
Marsh, D. McGahan, A. M. Saiful, B. Burhan, L. Siagian, D. Susanti, P.
D. Moi, M. Tocheri, A. R. Chivas, and A. Cahyana. F. Wesselingh
identified gastropod remains. Sidarto (GSI) provided digital elevation
model data used in Fig. 1b.
Geodetic surveys and measurements were conducted by E. E. Laksmana, A.
Rahmadi, Y. Sofyan, and G. Hazell. J. Noblett constructed the Mata Menge
3D model, based on drone aerial photographs taken by K. Riza, T. P.
Ertanto, and M. Faizal. The research team was supported by ~100
excavators and support personnel from the Ngada and Nage Keo districts.
We thank L. Kinsley, Research School of Earth Sciences, The Australian
National University, for assistance with mass spectrometric
measurements.
Author information
Author notes
- Adam Brumm
- , Gerrit D. van den Bergh
- & Iwan Kurniawan
- Michael J. Morwood
Affiliations
Research Centre of Human Evolution, Environmental Futures Research Institute, Griffith University, Nathan, Queensland 4111, Australia
- Adam Brumm
- & Rainer Grün
School of Earth & Environmental Sciences, University of Wollongong, Wollongong, New South Wales 2522, Australia
- Adam Brumm
Centre for Archaeological Science, School of Earth & Environmental Sciences, University of Wollongong, Wollongong, New South Wales 2522, Australia
- Gerrit D. van den Bergh
- , Brent V. Alloway
- , Ruly Setiawan
- , Dida Yurnaldi
- , Mika R. Puspaningrum
- , Unggul P. Wibowo
- , Thomas Sutikna
- & Michael J. Morwood
Quadlab, Natural History Museum of Denmark, University of Copenhagen, DK-1350 Copenhagen, Denmark
- Michael Storey
Geology Museum, Bandung 40122, Indonesia
- Iwan Kurniawan
- , Erick Setiyabudi
- , Unggul P. Wibowo
- , Halmi Insani
- , Indra Sutisna
- & Fachroel Aziz
School of Geography, Environment and Earth Sciences, Victoria University, Wellington 6012, New Zealand
- Brent V. Alloway
Center for Geological Survey, Geological Agency, Bandung 40122, Indonesia
- Ruly Setiawan
- & Dida Yurnaldi
Research School of Earth Sciences, The Australian National University, Canberra, Australian Capital Territory 2601, Australia
- Rainer Grün
Stone Tools and Cognition Hub, Archaeology, University of New England, Armidale, New South Wales 2351, Australia
- Mark W. Moore
Department of Earth Sciences, University of Toronto, Toronto, Ontario M5S 3B1, Canada
- John A. Westgate
Department of Geography & Earth Sciences, Aberystwyth University, Aberystwyth SY23 3DB, UK
- Nick J. G. Pearce
Geochronology, Centro Nacional de Investigación sobre la Evolución Humana (CENIEH), Paseo de Atapuerca, 3, 09002-Burgos, Spain
- Mathieu Duval
University Museum of Bergen, University of Bergen, 5007 Bergen, Norway
- Hanneke J. M. Meijer
Pusat Penelitian Arkeologi Nasional (ARKENAS), Jakarta 12510, Indonesia
- Thomas Sutikna
Cluster Earth & Climate, Faculty of Earth and Life Sciences, Vrije Universiteit, 1081 HV Amsterdam, The Netherlands
- Sander van der Kaars
School of Earth, Atmosphere and Environment, Monash University, Clayton, Victoria 3800, Australia
- Sander van der Kaars
School of Geosciences, The University of Edinburgh, Edinburgh EH8 9AD, UK
- Stephanie Flude
Contributions
A.B., G.D.v.d.B., I.K. and M.J.M. directed the Mata Menge excavations. M.S., B.V.A. and R.S. collected tephra samples and M.S. undertook 40Ar/39Ar dating. G.D.v.d.B. described the site stratigraphy, with R.S., D.Y., S.F. and B.V.A. ITPFT-dating of T3 was jointly conducted by J.A.W. and B.V.A., while EMP analyses of all So’a Basin tephra were conducted by B.V.A. and R.S. Comparative trace element analyses of interregional tephra markers were jointly undertaken by J.A.W., N.J.G.P. and B.V.A. E.S., F.A. and T.S. oversaw key aspects of the field project. M.W.M. analysed the stone assemblage, and G.D.v.d.B., H.I., I.S., M.R.P., U.P.W. and H.J.M.M. analysed the fauna. M.R.P. conducted isotopic analyses, R.G. and M.D. undertook U/Th and ESR analyses of faunal remains, and S.v.d.K. carried out the palynological analysis. A.B. and G.D.v.d.B. prepared the manuscript, with contributions from other authors.Competing interests
The authors declare no competing financial interests.Corresponding authors
Correspondence to Adam Brumm or Gerrit D. van den Bergh.Extended data
Extended data figures
- 1.
Hominin fossil find-locality at Mata Menge.
- 2.
Plan and baulk profiles of Excavation 32A-F showing distribution of finds.
- 3.
Glass shard geochemistry.
- 4.
40Ar/39Ar dating results.
- 5.
40Ar/39Ar dating results.
- 6.
40Ar/39Ar dating results.
- 7.
U-series and ESR samples and dating results.
- 8.
Carbon and oxygen isotope analysis of dental enamel.
- 9.
Analytical data for the Mata Menge stone technology.
Supplementary information
PDF files
- 1.
Supplementary Information
This file contains Supplementary Text and Data, Supplementary References, Supplementary Tables 1,3 and 6-8 and legends for Supplementary Tables 1-9 (see separate excel files for Supplementary Tables 2,4, 5 and 9)
Excel files
- 1.
Supplementary Table 2
Glass shard isothermal plateau fission-track (ITPFT) ages of T3 at both the Kopowatu (UT2382) and Lowo Mali (UT2383) sites within the So’a Basin (see Supplementary Information file for full legend). - 2.
Supplementary Table 4
Glass shard trace element analyses of T3 correlatives from Mata Menge, Lowo Mali and Kopowatu, and T6 from Mata Menge (see Supplementary Information file for full legend). - 3.
Supplementary Table 5
40Ar/39Ar dating results for Mata Menge samples (see Supplementary Information file for full legend). - 4.
Supplementary Table 9
Results of the pollen and phytolith analysis, Mata Menge (see Supplementary Information file for full legend).
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