Mutual Climatic Range (MCR) is a method of determining the past climate at an archaeological site by examining the tolerances of a range of species found there. One method is to find the average temperatures in January and July by looking at the modern distribution of beetle species found on the site.[1] Another application is to look at the tolerances of plant species to determine 'summer warmth and dryness' and 'wetness and winter warmth'.[2]

The technique was developed in the 1980s, and a newer one first published in 2009 which looks at geographical distribution is also sometimes called "mutual climatic range".[3]

References

  1. Ashton, Nick (2017). Early Humans. London: William Collins. p. 316. ISBN 978-0-00-815035-8.
  2. Sinka, J. J.; Atkinson, T. C. (1 March 1999). "A mutual climatic range method for reconstructing palaeoclimate from plant remains". Journal of the Geological Society. 156 (2): 381. Bibcode:1999JGSoc.156..381S. doi:10.1144/gsjgs.156.2.0381. S2CID 129041578.
  3. Lyman, R. Lee (15 July 2016). "The mutual climatic range technique is (usually) not the area of sympatry technique when reconstructing paleoenvironments based on faunal remains". Palaeogeography, Palaeoclimatology, Palaeoecology. Elsevier. 454: 75–81. Bibcode:2016PPP...454...75L. doi:10.1016/j.palaeo.2016.04.035.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.