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Pregled bibliografske jedinice broj: 76810

Cessation of karstification due to the sea-level rise? Case study of the Y-cave, Dugi Otok, Croatia


Juračić, Mladen; Bakran-Petricioli, Tatjana; Petricioli, Donat
Cessation of karstification due to the sea-level rise? Case study of the Y-cave, Dugi Otok, Croatia // Evolution of Karst: from Prekarst to Cessation / Gabrovšek, Franci (ur.).
Postojna : Ljubljana: Inštitut za raziskovanje krasa ZRC SAZU, Založba ZRC, 2002. str. 319-326 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)


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Naslov
Cessation of karstification due to the sea-level rise? Case study of the Y-cave, Dugi Otok, Croatia

Autori
Juračić, Mladen ; Bakran-Petricioli, Tatjana ; Petricioli, Donat

Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni

Izvornik
Evolution of Karst: from Prekarst to Cessation / Gabrovšek, Franci - Postojna : Ljubljana : Inštitut za raziskovanje krasa ZRC SAZU, Založba ZRC, 2002, 319-326

Skup
Evolution of Karst: from Prekarst to Cessation

Mjesto i datum
Postojna, Slovenija, 17.09.2002. - 21.09.2002

Vrsta sudjelovanja
Poster

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
sea-level; karstification; cave; submarine; erosion/corrosion; accumulation; submerged karst; endolithic and epilithic fauna; Adratic Sea

Sažetak
Along the eastern Adriatic coast a number of submerged karst phenomena are found (caves, submarine springs, poljes?) due to the recent (Late Pleistocene-Holocene) sea level rise of the order of 120 m. Formation of a submarine cave (Y-cave, 86 m long, entrance 6 - 12 m below sea level, with an air pocket above sea level) is discussed. Special attention was given to speleothems and recent corrosion in the remote shallow part of the cave. The role of endolithic and biomineralizing organisms is stressed.

Izvorni jezik
Engleski

Znanstvena područja
Geologija, Biologija



POVEZANOST RADA


Projekti:
0119402
119301

Ustanove:
Prirodoslovno-matematički fakultet, Zagreb


Citiraj ovu publikaciju:

Juračić, Mladen; Bakran-Petricioli, Tatjana; Petricioli, Donat
Cessation of karstification due to the sea-level rise? Case study of the Y-cave, Dugi Otok, Croatia // Evolution of Karst: from Prekarst to Cessation / Gabrovšek, Franci (ur.).
Postojna : Ljubljana: Inštitut za raziskovanje krasa ZRC SAZU, Založba ZRC, 2002. str. 319-326 (poster, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
Juračić, M., Bakran-Petricioli, T. & Petricioli, D. (2002) Cessation of karstification due to the sea-level rise? Case study of the Y-cave, Dugi Otok, Croatia. U: Gabrovšek, F. (ur.)Evolution of Karst: from Prekarst to Cessation.
@article{article, author = {Jura\v{c}i\'{c}, Mladen and Bakran-Petricioli, Tatjana and Petricioli, Donat}, editor = {Gabrov\v{s}ek, F.}, year = {2002}, pages = {319-326}, keywords = {sea-level, karstification, cave, submarine, erosion/corrosion, accumulation, submerged karst, endolithic and epilithic fauna, Adratic Sea}, title = {Cessation of karstification due to the sea-level rise? Case study of the Y-cave, Dugi Otok, Croatia}, keyword = {sea-level, karstification, cave, submarine, erosion/corrosion, accumulation, submerged karst, endolithic and epilithic fauna, Adratic Sea}, publisher = {In\v{s}titut za raziskovanje krasa ZRC SAZU, Zalo\v{z}ba ZRC}, publisherplace = {Postojna, Slovenija} }
@article{article, author = {Jura\v{c}i\'{c}, Mladen and Bakran-Petricioli, Tatjana and Petricioli, Donat}, editor = {Gabrov\v{s}ek, F.}, year = {2002}, pages = {319-326}, keywords = {sea-level, karstification, cave, submarine, erosion/corrosion, accumulation, submerged karst, endolithic and epilithic fauna, Adratic Sea}, title = {Cessation of karstification due to the sea-level rise? Case study of the Y-cave, Dugi Otok, Croatia}, keyword = {sea-level, karstification, cave, submarine, erosion/corrosion, accumulation, submerged karst, endolithic and epilithic fauna, Adratic Sea}, publisher = {In\v{s}titut za raziskovanje krasa ZRC SAZU, Zalo\v{z}ba ZRC}, publisherplace = {Postojna, Slovenija} }




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