Advanced computer modelling of hominin dispersal from Africa: integrating archaeological and palaeoclimatic simulations

Paul Valdes, Steven Mithen, Bruce Sellwood, John Hughes, Sam Smith, Alan Haywood, 2007. https://doi.org/10.5284/1000212. How to cite using this DOI

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https://doi.org/10.5284/1000212
Sample Citation for this DOI

Paul Valdes, Steven Mithen, Bruce Sellwood, John Hughes, Sam Smith, Alan Haywood (2007) Advanced computer modelling of hominin dispersal from Africa: integrating archaeological and palaeoclimatic simulations [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1000212

Data copyright © Prof Paul Valdes unless otherwise stated

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Primary contact

Prof Paul Valdes
School of Geographical Sciences
University of Bristol
43 Woodland Road
Bristol
BS8 1UU
UK

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Resource identifiers

Digital Object Identifiers

Digital Object Identifiers (DOIs) are persistent identifiers which can be used to consistently and accurately reference digital objects and/or content. The DOIs provide a way for the ADS resources to be cited in a similar fashion to traditional scholarly materials. More information on DOIs at the ADS can be found on our help page.

Citing this DOI

The updated Crossref DOI Display guidelines recommend that DOIs should be displayed in the following format:

https://doi.org/10.5284/1000212
Sample Citation for this DOI

Paul Valdes, Steven Mithen, Bruce Sellwood, John Hughes, Sam Smith, Alan Haywood (2007) Advanced computer modelling of hominin dispersal from Africa: integrating archaeological and palaeoclimatic simulations [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1000212

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Project Aims

The project aim was to develop process-based computer simulations of the dispersal of Homo erectus out of Africa. This involved developing realistic constraints on the patterns of vegetation and the effects of changes in global sea level. It was assumed that this migration out of Africa could be investigated through the paradigm of a single migration event, starting around 2 millions of years ago and arriving in Dmanisi around 1.8 millions of years ago.

Archive description

The data archived here consists of the vegetation patterns used in constructing the simulations and the patterns of climate variability used to constrain the variations in sea level and vegetation change. From these data it is possible to reproduce the simulation results. Simulation results are available from:

J.K. Hughes, A. Haywood, S.J. Mithen, B.W. Sellwood, P.J. Valdes (In Press) 'Investigating Early Hominin Dispersal Patterns: developing a framework for climate data integration'. Journal Of Human Evolution.

The land distribution and orography used were from the ICE-4G data set, and can be obtained through the USGS from: http://geo-nsdi.er.usgs.gov/metadata/other/pages-93-015/metadata.faq.html

  • File 1 - Climate_variability.csv - contains three alternative climate variability records implemented (corresponding to a plio-pleistocene vegetation transitions at 2.5, 1.8 and 1.0 Mya). This record is based on benthic foram data from the Delphi project (http://www.esc.cam.ac.uk/delphi/).
  • File 2 - Climate_var_modern.csv - contains the climate variability data set used in modern Homo sapiens simulations, derived from the Vostok ice core (http://cdiac.ornl.gov/ftp/trends/co2/vostok.icecore.co2).
  • File 3 - Vegetation.txt - contains the vegetation patterns used in Stepping Out. To read in the data from this file use the following Fortran code structure:

    OPEN (14,file='Vegetation.txt')
    DO I=1,12
    DO X=1,360
    DO Y=1,180
    READ(14,*) Veg(X,Y,I)
    ENDDO
    ENDDO
    ENDDO
    CLOSE(14)

The index level 'I' to be used at a particular time step is then specified by the Climate_variability.csv value. These vegetation distributions were derived from climate model (GCM) simulations of glacial to interglacial climate variability (1-11, 1=glacial) and of the mid-pliocene warm period (12). It is strongly recommended that anyone intending to make use of these vegetation data contact Professor Valdes of Bristol University (p.j.valdes@bristol.ac.uk) to discuss the nature of these vegetation patterns and the process-based modelling that produced them. The science behind the climate model simulations are, at present, rapidly developing and it is expected that the vegetation patterns will be superceded in the near future. Vegetation codes correspond to 1) tropical forest, 2) warm-temperate forest, 3) temperate forest, 4) boreal forest, 5) savannah and dry woodland, 6) grassland and dry shrubland, 7) desert, 8) tundra, 9) land ice and 10) ocean.

In the dispersal modelling the sequence of events was:

  • Initialisation
  • Start of main loop
  • Colonisation
  • Extinction
  • Preliminary output
  • End of main loop
  • Final output

Files

Climate_variability.csv CSV
Climate_variability.csv
Climate_variability.csv
[DOWNLOAD] right-click and save link
202 Kb
Climate_var_modern.csv CSV
Climate_var_modern.csv
Climate_var_modern.csv
[DOWNLOAD] right-click and save link
7 Kb
Vegetation.txt TXT
Vegetation.txt
Vegetation.txt
[DOWNLOAD] right-click and save link
9.64 Mb



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