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Mavro

Variety of grape


Summary

Variety of grape

FieldValue
nameMavro (μαύρο)
imageMavro.jpg
captionMavro grapes
speciesVitis vinifera
originCyprus
hazards
notable_winesCommandaria

Mavro (, meaning "black") is an indigenous red grape cultivated on the island of Cyprus. The grape takes its name from its dark colour. The Italian ampelographer, Count Giuseppe di Rovasenda refers to it in 1877 as Cipro Nero (Cyprus black). An ancient variety, its suitability to the hot Cypriot climate has made it the dominant cultivated vine on the island. It accounts for 70% of cultivated vines. Of note is that Mavro continues to grow on ancient rootstock unlike most mainland European grapes that are grafted on North American rootstock. This is a consequence of Cyprus’ escape from the phylloxera epidemic that had devastated most other European vineyards, in the 19th century.

Mavrud is a Bulgarian wine with a similar name made from mavrud grapes. Recent genotyping has shown that these two varieties (Mavro and Mavrud) are not related.

Mavro grapes are used in the production of several (predominantly red) local wines. It is also used in the production of the spirit zivania. Harvesting usually takes place in September.

References

References

  1. "Κρασί κυπριακό : Μια παράδοση 5500 χρόνων". Cyprus Food Virtual Museum.
  2. di Rovasenda, Giuseppe. (1877). "Saggio di Ampelografia Universale (Essay on Universal [[Ampelography]])".
  3. ''page 454, Larousse Encyclopaedia of Wine by Christopher Foulkes, {{ISBN. 0-600-60475-6.''
  4. (13 January 1994). "Cyprus wine comes of age". CatererSearch.
  5. Hvarleva, T. (2005). "Genotyping Vitis vinifera L. cultivars of Cyprus by microsatellite analysis.". Vitis.
  6. (13 March 2014). "Οι δρόμοι του κρασιού στη Μεγαλόνησο". To Vima.
  7. Meuse, Stephen. (June 6, 2010). "Winemaking in transition". [[The Boston Globe]].
  8. "Zivana (zivania) product description". LOEL Ltd.
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This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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