2008
Woch, M. W.; Mueller-Bieniek, A.; Urbisz, A.
In: Fragmenta Floristica et Geobotanica Polonica, vol. 15, no. 2, pp. 223-230, 2008, ISSN: 1640629X, (2).
@article{2-s2.0-84866082750,
title = {Glaucium corniculatum (Papaveraceae) - A medieval ephemerophyte in the Polisch flora [Glaucium corniculatum (Papaveraceae) - Średniowieczny efemerofit we florze polskiej]},
author = { M.W. Woch and A. Mueller-Bieniek and A. Urbisz},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-84866082750&partnerID=40&md5=723811abdb725fea40bc60700bece224},
issn = {1640629X},
year = {2008},
date = {2008-01-01},
journal = {Fragmenta Floristica et Geobotanica Polonica},
volume = {15},
number = {2},
pages = {223-230},
abstract = {The paper presents finding of Glaucium comiculatum seeds in sediments of medieval Cracow. In contemporary Polish flora this species has ephemerophyte status of MediterraneanIranian-Turanian origin. It has been noted at railway habitats, and more rarely in segetal habitats. In samples where G. comiculatum was found, species of thermophilic segetal and ruderal assemblages associated with subcontinental climate were dominated; characterized by high thermal, trophy and acidity values, as well as low moisture and soil granulomere values. This suggests that this species might have remained in assemblages present in medieval ages. Probably the species was being constantly spread, and climatic conditions might have supported its persistence. Contemporary distribution map in a cartogramme version is presented.},
note = {2},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The paper presents finding of Glaucium comiculatum seeds in sediments of medieval Cracow. In contemporary Polish flora this species has ephemerophyte status of MediterraneanIranian-Turanian origin. It has been noted at railway habitats, and more rarely in segetal habitats. In samples where G. comiculatum was found, species of thermophilic segetal and ruderal assemblages associated with subcontinental climate were dominated; characterized by high thermal, trophy and acidity values, as well as low moisture and soil granulomere values. This suggests that this species might have remained in assemblages present in medieval ages. Probably the species was being constantly spread, and climatic conditions might have supported its persistence. Contemporary distribution map in a cartogramme version is presented.