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master's thesis
Taložni okoliši i foraminiferske zajednice u sedimentima delte rijeke Mirne
Zagreb: University of Zagreb, Faculty of Science, 2017. urn:nbn:hr:217:490060
Vinković, Andrija
University of Zagreb
Faculty of Science
Department of Geology

Institutional repository: Repository of the Faculty of Science

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Vinković, A. (2017). Taložni okoliši i foraminiferske zajednice u sedimentima delte rijeke Mirne (Master's thesis). Zagreb: University of Zagreb, Faculty of Science. Retrieved from https://urn.nsk.hr/urn:nbn:hr:217:490060

Vinković, Andrija. "Taložni okoliši i foraminiferske zajednice u sedimentima delte rijeke Mirne." Master's thesis, University of Zagreb, Faculty of Science, 2017. https://urn.nsk.hr/urn:nbn:hr:217:490060

Vinković, Andrija. "Taložni okoliši i foraminiferske zajednice u sedimentima delte rijeke Mirne." Master's thesis, University of Zagreb, Faculty of Science, 2017. https://urn.nsk.hr/urn:nbn:hr:217:490060

Vinković, A. (2017). 'Taložni okoliši i foraminiferske zajednice u sedimentima delte rijeke Mirne', Master's thesis, University of Zagreb, Faculty of Science, accessed 22 November 2024, https://urn.nsk.hr/urn:nbn:hr:217:490060

Vinković A. Taložni okoliši i foraminiferske zajednice u sedimentima delte rijeke Mirne [Master's thesis]. Zagreb: University of Zagreb, Faculty of Science; 2017 [cited 2024 November 22] Available at: https://urn.nsk.hr/urn:nbn:hr:217:490060

A. Vinković, "Taložni okoliši i foraminiferske zajednice u sedimentima delte rijeke Mirne", Master's thesis, University of Zagreb, Faculty of Science, Zagreb, 2017. Available at: https://urn.nsk.hr/urn:nbn:hr:217:490060

Metadata
TitleTaložni okoliši i foraminiferske zajednice u sedimentima delte rijeke Mirne
Title (english)Depositional environments and foramiferal assemblages in sediments of the Mirna River delta
AuthorAndrija Vinković
MentorMladen Juračić (mentor)
Committee memberMladen Juračić (predsjednik povjerenstva)
Committee memberBlanka Cvetko Tešović (član povjerenstva)
Committee memberMarijan Kovačić (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Science
(Department of Geology)
Zagreb
Defense date and country2017-09-25, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Geology and Paleontology
Abstract
Foraminiferska analiza provedena je na šest jezgri duljine od 7,5 do 13 m izvađenih iz deltne ravnice rijeke Mirne. Za mikropaleontološku analizu primijenjen je FOBIMO protokol. U svim jezgrama određeni su apsolutni broj foraminifera, relativni postotak i indeksi bioraznolikosti (Shannonov, indeks dominacije, Simpsonov, Berger-Parkerov i Fisher α). Najplići dijelovi jezgara ne sadrže foraminifere. Najdominantnije vrste u dubljim intervalima pripadaju rodovima Ammonia, Haynesina i Porosononion. U dubljim intervalima, smanjuje se njihova zastupljenost i pojavljuju se jedinke roda Elphidium te miliolida. Povećanjem dubine, marinski utjecaj u jezgrama se povećava i indeksi bioraznolikosti pokazuju sve manju dominaciju pojedinih rodova. Prema zastupljenosti navedenih rodova i varijacija u indeksima bioraznolikosti, prepoznati su slijedeći taložni okoliši: aluvijalni okoliši, brakični okoliši (močvare/lagune), unutrašnji estuariji, središnji i vanjski estuariji. Promjena vertikalnih taložnih okoliša zbog horizontalnog pomaka rijeke ukazuje na progradaciju tijekom holocena.
Abstract (english)
Foraminiferal analysis was carried out on six cores down to the depth from 7.5 to 13 m. from the Mirna River deltaic plain. FOBIMO protocol was used for micropaleontological analysis. For all cores absolute abundance, relative abundance and biodiversity indices (Shannon, Dominance, Simpson, Berger-Parker and Fisher's alpha) were calculated. Foraminifera in the shallowest intervals are completely lacking. In the deeper intervals dominant species belong to Ammonia, Haynesina and Porosononion genus. In deeper intervals, their abundance is reduced and individuals belonging to Elphidium genus and miliolids start to appear. Marine influence became more pronounced with depth and biodiversity indices have shown a decreasing dominance of certain genera. According to the abundance of said genera and variation of biodiversity indices, the following depositional environments were suggested: alluvial environments, brackish environments (marshes/lagoons), inner estuaries, central and outer estuaries. Changes in vertical depositional environments caused by horizontal river movement indicate progradation during Holocene.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:217:490060
Study programmeTitle: Graduate university study of Geology
Study programme type: university
Study level: graduate
Academic / professional title: magistar/magistra geologije (magistar/magistra geologije)
Type of resourceText
File originBorn digital
Access conditionsOpen access
Terms of useLicence In copyright icon
Created on2018-01-29 14:31:50