Kazan Federal University Digital Repository

Climate changes and human impact on the Mistras coastal barrier system (W Sardinia, Italy)

Show simple item record

dc.contributor.author Pascucci V.
dc.contributor.author De Falco G.
dc.contributor.author Del Vais C.
dc.contributor.author Sanna I.
dc.contributor.author Melis R.
dc.contributor.author Andreucci S.
dc.date.accessioned 2019-01-22T20:33:21Z
dc.date.available 2019-01-22T20:33:21Z
dc.date.issued 2018
dc.identifier.issn 0025-3227
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/147694
dc.description.abstract © 2017 Elsevier B.V. Integrated archaeological and geological studies conducted on Mistras coastal barrier system of central Sardinia showed that it developed as transgressive systems during the final stages of the Holocene sea level rise (final stage of the Holocene Climate Optimum, about 6300–6000 cal y BP), and become regressive (prograding) from about 2500 cal y BP, when sea level reached the present elevation. The regression of the coast was, however, not continuous, but characterized by distinct Transgressive-Regressive phases (T-R), associated to precise climatic fluctuations, tied with global eustatic and climatic phases. The first regression occurred between 2500 and 1900 cal y BP. This time interval, known as Roman Warm, coincides with the Phoenician, Punic and Roman attendance of the west Sardinia coast. At that time, areas close to the coastal cities had to host landings and perhaps ports probably located at short distance from the shoreline. Archaeological excavations and findings have documented that in the Mistras area Punic constructed a long boulder structure (probably dated from the 4th century BCE) to better protect an incipient lagoon used as the harbour of the city of Tharros. This had the effect to modify the normal behaviour of the beach system that transformed from spit to barrier lagoon. During the second regressive phase, the well-established beach lagoon system developed quasi continuously for > 1200 y (650 and 1850 CE). This progradation started during a new warm period (Medieval) and continued favoured by gentle sea level fall occurred during the cold Little Ice Age time. During this time, after the abandonment of the city of Tharros and of the Sinis Peninsula, the Mistras area was poorly populated. As consequence, there was no more an active harbour and large sandy dunes developed and nourished the shore allowing a no man-influence progradation of the coast. The third stage is the current one and begun about 165 y ago (post 1850 CE) after the relative sea level rise occurred after the end of the Little Ice Age. Geological and archaeological data of western Sardinia barrier lagoon systems revealed that the Mistras barrier lagoon evolution was human influenced since the Punic time. The study pointed that little human activities on the coast could influence its natural behaviour and landscape, and that little climatic changes both positive and negative can induce progradation or erosion of the system as well.
dc.relation.ispartofseries Marine Geology
dc.subject Holocene
dc.subject Millennial scale transgressive-regressive cycles
dc.subject Punic harbour
dc.subject Roman warm time
dc.subject Sinis Peninsula
dc.subject Tharros
dc.title Climate changes and human impact on the Mistras coastal barrier system (W Sardinia, Italy)
dc.type Article
dc.relation.ispartofseries-volume 395
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 271
dc.source.id SCOPUS00253227-2018-395-SID85034059446


Files in this item

This item appears in the following Collection(s)

  • Публикации сотрудников КФУ Scopus [24551]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

Show simple item record

Search DSpace


Advanced Search

Browse

My Account

Statistics