аЯрЁБс>ўџ 8:ўџџџ7џџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџьЅС5@ №ПшbjbjЯ2Я2 .­X­XшџџџџџџˆШШШШШШШўЂЂЂЂ Ў ў(ЦЦЦЦЦЁЁЁ‡‰‰‰‰‰‰$<RŽ L­!ШЁЁЁЁЁ­ШШЦЦлЮПППЁpШЦШЦ‡ПЁ‡ППзШШзЦК №Z„‚ЌгЂ(з{ ф0зк 9к зм№ШШШШзhк Ш?<ЁЁПЁЁЁЁЁ­­ўўЄЂOpўўЂUse of Geological Maps and Geological Mapping as an Aid in the Study of the Plant World and the Possibility of Using Botanical Spatial Data in Geology Sonja `I`I, Marko RANDI, Nina TRINAJSTI, Dino GROZI Public Institution Priroda, Grivica 4, 51000 Rijeka, Croatia marko.randic@ju-priroda.hr Abstract By studying grassland vegetation on the slopes of the mountains in the hinterland of Rijeka town, Croatia we have observed that some types of grasslands show a clear regularity of spatial distribution in relation to the types of carbonate geological substrates. This is particularly true for Mediterranean-mountain grasslands dominated by narrow-leaved moor grass (Sesleria juncifolia). The geological bedrock, of course, with other climatic factors (strong bora wind!) is one of the possible ecological factors that could help clarify and delimit certain vegetation units within a wider set of communities with the narrow-leaved moor grass (Seslerietum juncifolie s. l.). Some of the communities from this complex are closely related to the dolomite, others to the limestone, and some to the glacial sediments (till). Using the available vegetation maps, pedological maps, geological maps and satellite imagery, we have tried to elaborate a methodology of comparative geological and vegetation mapping that would help to throw light on the relationship between the geological substrate and the type of grassland vegetation. Comparative study and mapping of geological substrate and vegetation could find practical application as an aid in geological exploration, but also in studying and mapping vegetation. Keywords: comparative study of vegetation and geology, geological maps, vegetation maps, grassland vegetation, dolomite, limestone, glacial sediment  , . 0 < F V b p „ ’ ž В Ж И ж к   ( * 2 4 Ё Д Ж в › œ Ќ ­ P[цшїяїыфнфнфнфныфйфыфывыфыфЪфЪфЦфЦфыфыhмZіhмZіhЫ;В6 hтhтhn_ hтh`Sh hтhЫ;ВhтhтhЫ;В5hтhт5#. 0   Ђ  ) * 3 4 QRчшњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!ЌњР!Ќgdт ш§,1hАа/ Ар=!А"А# $ %ААФАФ ФœD@ёџD NormalCJ_HaJmH nHsH tHDAђџЁD Default Paragraph FontRiѓџГR  Table Normalі4ж l4жaі (kєџС(No List H™@ђH мZі0 Balloon TextCJOJQJ^JaJFўђџF мZі0 Char$CJOJQJ^JaJmH nHsH tHшџџџџш—˜аб)*34QRчъ˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€˜0€€шш ш №8№@ёџџџ€€€ї№’№№0№( № №№B №S №ПЫџ ?№žЃЋБИТЩЯлм›œЌ­[[цъ›œЌ­чъ4ъžЃЋБИТЩЯлм›œЌ­[[цъџџLapaine "f Ѕi'Ѕi'^{:>VX’'Б_,rЭ*Ÿ6 "f ^{:>N:3sБ_,rЭ*Ÿ6N:3s хтѕdщ+-дFG`ee`Shn_Ы;ВмZіъџ@€а$шpp@џџUnknownџџџџџџџџџџџџG‡z €џTimes New Roman5€Symbol3& ‡z €џArial;†SimSun‹[SO5& ‡za€џTahoma"1ˆ№аhЯ…Xgр™XЧс с С№ ДД4хх3ƒQ№џ§HP рџ?фџџџџџџџџџџџџџџџџџџџџџщ+-џџ~Title of the presentation:: Use of geological maps and geological mapping as an aid in the study of the plant world and the poLapaine Ivka Kljajiўџр…ŸђљOhЋ‘+'Гй0ј$˜ ,<HX p| ˜ Є АМФЬдмщ§Title of the presentation:: Use of geological maps and geological mapping as an aid in the study of the plant world and the poitlLapaineapaNormalIvka KljajiФ‡re3kaMicrosoft Word 10.0@Œ†G@ЂИдг@ђzЌгсG#џџџџVT$m€ y‘  въ.ћœџМ@Times New Roman- †2 ДюRьШUse of Geological Maps and Geological Mapping as an Aid in the Study of the Plant H',2"M,222,2^28(288M,222,2^288822'28H88!8,8!8722"!8,<28!h2 'ю>ьШWorld and the Possibility of Using Botanical Spatial Data in Gd2,8288!8,<2''8!22"H'82C2!28,2782!2H2!28M2 'S ьШeology,2222 2 'cьШ 6ћœџ@Times New Roman- 2 ˜юьШ -2 юьШSonja 822, ыћœџю@Times New Roman-.2 ыьШŠIŠIЦ 99C.-№2 оьШ, Marko Z,!22 4ћœџю@Times New Roman-.2 4ьШRANDIЦCIHIC.-№2 ГьШ, Nina H2, Сћœџю@Times New Roman-.2 С ьШTRINAJSTIЦ=D HH(8> C.-№2 ѓ ьШ, Dino H22  ћœџю@Times New Roman-.2  ьШGROZIЦHCH= C.-№ 2 y ьШ . 2 ~юьШ -2 ёюьШPublic I822,2 ё'ьШns2' 2 ё€ьШt"2 ёœьШitution Priroda2228!!22,2 ёсьШ, (2 ёьШGrivica 4, 51000 RiH!2,,222222C2 ё- ьШjeka,2-2 ёд ьШ, CroatiarC!2,, 2 ё, ьШ -"2 dюьШmarko.randic@juN,!22!,22,\3 2 dЊьШ-!2 dЫ ьШpriroda.hr2!!22-2! 2 dXьШ - 2 зюьШ -2 JюьШAbstractH2'!,, 2 J@ьШ . 2 НюьШ -‹2 0юUьШBy studying grassland vegetation on the slopes of the mountains in the hinterland of D0'230312!,'',222-1,,22222,'22,'2!2,N222,2'22,22,!,222!…2 ЃюQьШRijeka town, Croatia we have observed that some types of grasslands show a clear C,2,2H2C!2,,H,2,2,22',!3,22,'2N,02,'2!2!,'',22''22H,,,-!D2 ю&ьШregularity of spatial distribution in !-12,!02!'2,,2'!22222b2 d:ьШrelation to the types of carbonate geological substrates. !,,2222,03,'3!,-!222,,2,222,,'22'!,,'L2 ‰ю+ьШThis is particularly true for Mediterranean=2''2,!,2,!0!2,"2!Y,2,!",2,,3 2 ‰ƒ ьШ-!F2 ‰Є 'ьШmountain grasslands dominated by narrowN222,21",'',22'22N2,,3302-!!2I 2 ‰HьШ-"ћœџ@Times New Roman--(2 ќюьШleaved moor grass (,,2,2N22!1",''!-(2 ќџьШSesleria juncifolia2,'-'222,22-U2 ќл1ьШ). The geological bedrock, of course, with other !=2,1,231-,2,2!2,23!,22!(,H222,!42 o юьШclimatic factors (strong bo.,N,,!,,2!'!'!23132j2 o ?ьШra wind!) is one of the possible ecological factors that could !,H22!!'22,3!2,32''2,,,221,,!-,2!(2,,222‘2 т юYьШhelp clarify and delimit certain vegetation units within a wider set of communities with 2,2,,!#0,222,N,,!,22-1,,2222'H22,H2,!',2!,2NO22,'H2-2 U ю ьШthe narrow2,2,!!2I 2 U œьШ-!(2 U НьШleaved moor grass (,,3,2N22!1",''!-52 U ЯьШSeslerietum juncifolie s. l.2,',',2H23,2,'-42 U м ьШ). Some of the communities .!82N,2!2,,3NN22,'(2 Ш юьШfrom this complex a!!2N2',2N2,3,t2 Ш FьШre closely related to the dolomite, others to the limestone, and some !,,2',0",,,222,223N,22,!'22,N,'22,,22'2N,‹2 ; юUьШto the glacial sediments (till). Using the available vegetation maps, pedological map 22,1-,,',2N,2'"!H'212,,2,,2,2,2,,22N,2'2,2231-,N,2 2 ; ьШs'2 ; 2ьШ,  2 Ў юьШgeological map1,231-,N,2 2 Ў SьШs'q2 Ў zDьШ and satellite imagery, we have tried to elaborate a methodology of ,22',-,N,1,#0I,2,3,!,22,,22!,,,N,22322302!"2 ! юьШcomparative geo,2N2,!,2,2,2s2 ! …EьШlogical and vegetation mapping that would help to throw light on the 21,,-222,2,,22N,22312,H2222,222!2H12222,‰2 ” юTьШrelationship between the geological substrate and the type of grassland vegetation. !,,22'222,H,,23,1,231-,'22'!,,,222,03,2!1",'',222-1-,22ƒ2  юPьШComparative study and mapping of geological substrate and vegetation could find C2N2,!,2,'230,22N,22212!2,221,,'32'!,,,222-2,,22,322!22.2 z юьШpractical application a2!,,,,,22,,22,s2 z `EьШs an aid in geological exploration, but also in studying and mapping '-2,221,231-,,322!,2222,'22'23/31,22O,22212 э ю ьШvegetation. 2,2,,22 2 э ЇьШ . 2 `юьШ -2 гю ьШKeywords:H.0H2!2'z2 гЄJьШ comparative study of vegetation and geology, geological maps, vegetation ,2N2-!,2,(2302!3-1,,22,221-22301,231-,N,2'2,2,,22m2 FюAьШmaps, grassland vegetation, dolomite, limestone, glacial sedimentiN,2'1",'',222-2,,22222N,N,'22,1-,,',2N,2 2 F0 ьШ . 2 ЙюьШ -ћМ"System`єjф-ШШььЧЧыыЦЦъъХХщщФФшшУУччТТццССххРРфф П Пу у  О От т  Н Нс с  М Мр р  Л Лп п ККооЙЙннИИммЗЗллЖЖккўџеЭеœ.“—+,љЎ0x hpŒ”œЄ ЌДМФ Ь WфGeodetski fakultet хA Title of the presentation:: Use of geological maps and geological mapping as an aid in the study of the plant world and the po Title ўџџџ ўџџџўџџџ !"#$%&'()*+,-.ўџџџ0123456ўџџџ§џџџ9ўџџџўџџџўџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџRoot Entryџџџџџџџџ РF№Z„‚Ќг;€Data џџџџџџџџџџџџ 1TableџџџџWordDocumentџџџџ.SummaryInformation(џџџџџџџџџџџџ(%DocumentSummaryInformation8џџџџџџџџ/CompObjџџџџџџџџџџџџjџџџџџџџџџџџџўџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџџўџ џџџџ РFMicrosoft Word Document MSWordDocWord.Document.8є9Вq