GEOARCHAEOLOGICAL EVIDENCE OF LATE AND POSTANTIQUITY (5TH–9TH C. AD) CLIMATE CHANGES RECORDED AT THE ROMAN SITE IN PLEMIĆI BAY (ZADAR REGION, CROATIA)
Journal Title: Studia Quaternaria - Year 2019, Vol 36, Issue 1
Abstract
Remains of a vast Roman pottery production complex were found on the shore of the Plemići Bay (Općina Ražanac, Zadar county) in 2012, and confirmed by geophysical survey. Ground-penetrating radar measurements revealed outline of a rectangular building that finds analogies with Roman storehouses (horreum). The area occupied by remains of the Roman pottery workshop was covered by immense soil-debris flows. Three geological exposures located to the north of the remains of the Roman building were documented using lithological and malacological analysis, and magnetic susceptibility measurements. The profiles revealed at least three generations of slope sediments, formed in result of intensive soil or debris flows in a dry climate, most probably in 5th c. AD. In the next, wet phase sediments were transported downslope and deposited on the Roman structures after 5th c. AD. Environmental conditions at Pelmići were supply with paleoclimate evidence from the Adriatic region. At ca. 1.5 cal. BP lake levels in the eastern Adriatic area were drastically reduced, probably because of strong decrease in humidity, correlated with the so-called North Atlantic Bond event 3. The drought was followed by a humid episode, also attested at the Plemići archaeological site.
Authors and Affiliations
Fabian Welc
VEGETATION AND STRATIGRAPHY OF THE MAZOVIAN (HOLSTEINIAN) INTERGLACIAL SECTIONS FROM DOBROPOL AND OTHER NEW SITES IN WESTERN POLESIE REGION, SOUTH-EASTERN POLAND
Geological mapping in eastern Poland resulted in new find of organic deposits near Włodawa. Pollen and plant macrofossils analyses at the Dobropol site proved deposition during the Mazovian (Holsteinian) Interglacial (MI...
ORIGIN AND EVOLUTION OF BASINS IN THE EASTERN PART OF JASŁO-SANOK DEPRESSION (POLISH CARPATHIANS) IN THE LATE VISTULIAN AND HOLOCENE
Results of a geomorphologic study as well as radiocarbon and pollen analyses of sediments in small basins of the Jasło-Sanok Depression (Western Carpathians) are summarised. Floors of these basins, carved in soft shale-s...
LAST TWO MILLENNIA WATER LEVEL CHANGES OF THE LAKE MŁYNEK (NORTHERN POLAND)INFERRED FROM DIATOMS AND CHRYSOPHYTE CYSTS RECORD
A sediment core, 350 cm long recovered from Młynek Lake, northern of Poland (Warmia and Masuria Region) was analyzed with respect to their content of diatoms and chrysophyte cysts. The aim was to reconstruct the lake wat...
QUATERNARY VALLEY LEVELS AND RIVER TERRACES IN THE WESTERN PART OF THE HOLY CROSS MOUNTAINS
According to the current state of research five sand-gravel accumulation levels of Quaternary age are visible in the morphology of the western part of the Holy Cross Mountains, within the Wierna Rzeka, Hutka and Bobrza r...
CHRONOSTRATIGRAPHY OF THE LATE VISTULIAN IN CENTRAL POLAND AND THE CORRELATION WITH VISTULIAN GLACIAL PHASES
The Vistulian decline was a period of rapid environmental events. The authors correlated ages of the last Scandinavian Ice Sheet limits in northern Poland with ages of prominent events adapting the conditions of periglac...