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{\title NASLOV POVZETKA}{\author Uro\'9a Er\'9een}{\operator karmen}{\creatim\yr2006\mo7\dy21\hr15\min52}{\revtim\yr2006\mo7\dy21\hr15\min52}{\version2}{\edmins0}{\nofpages1}{\nofwords575}{\nofchars3281}{\*\company R\'8eS}{\nofcharsws3849}
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\pnlcrm\pnstart1\pnindent720\pnhang {\pntxtb (}{\pntxta )}}\pard\plain \ltrpar\s17\ql \li0\ri0\sa240\widctlpar\pvpara\posy0\dxfrtext142\dfrmtxtx142\dfrmtxty142\wraparound\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0\pararsid7039412 \rtlch\fcs1 
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TINCTION AT THE VELEBIT Mt.}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412\charrsid16713565 , CROATIA: GEOCHEMICAL AND ISOTOPICAL INSIGHTS}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412 
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\af0 \ltrch\fcs0 \insrsid7039412 Fio, K.}{\rtlch\fcs1 \af0\afs24 \ltrch\fcs0 \super\insrsid7039412\charrsid7039412 1,2}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412 , Spangenberg, J.}{\rtlch\fcs1 \af0\afs24 \ltrch\fcs0 
\super\insrsid7039412\charrsid7039412 1}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412 , Sremac, J.}{\rtlch\fcs1 \af0\afs24 \ltrch\fcs0 \super\insrsid7039412\charrsid7039412 2}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412 , Vlahovi\'e6, I.}{\rtlch\fcs1 
\af0\afs24 \ltrch\fcs0 \super\insrsid7039412\charrsid7039412 3}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412 , Veli\'e6, I.}{\rtlch\fcs1 \af0\afs24 \ltrch\fcs0 \super\insrsid7039412\charrsid7039412 3}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412 
 and Mrinjek, E.}{\rtlch\fcs1 \af0\afs24 \ltrch\fcs0 \super\insrsid7039412\charrsid7039412 2
\par }\pard\plain \ltrpar\s19\ql \li0\ri0\sa120\widctlpar\wrapdefault\aspalpha\aspnum\faauto\adjustright\rin0\lin0\itap0\pararsid6901290 \rtlch\fcs1 \af0\afs20\alang1025 \ltrch\fcs0 \fs20\lang1024\langfe1024\cgrid\noproof\langnp1050\langfenp1050 {\rtlch\fcs1 
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{\*\xmlopen\xmlns1{\factoidname City}}{\*\xmlopen\xmlns1{\factoidname place}}University of Lausanne{\*\xmlclose}, {\*\xmlopen\xmlns1{\factoidname country-region}}Switzerland{\*\xmlclose}{\*\xmlclose}; Jorge.Spangenberg@unil.ch
\par }{\rtlch\fcs1 \af0 \ltrch\fcs0 \cs23\scaps\super\insrsid7039412 2 }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412 Department of Geology and Paleontology, University of Zagreb, Croatia; }{\field\flddirty{\*\fldinst {\rtlch\fcs1 \af0 \ltrch\fcs0 
\insrsid7039412\charrsid13439343  HYPERLINK "mailto:karmen.fio@gmail.com" }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412\charrsid13439343 {\*\datafield 
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\ltrch\fcs0 \insrsid7039412\charrsid13439343  HYPERLINK "mailto:jsremac@gmail.com" }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412\charrsid13439343 {\*\datafield 
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\ltrch\fcs0 \insrsid10249564 .mrinjek@zg.t-com}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412 .hr
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Croatian Geological Survey, Zagreb, Croatia; }{\field\flddirty{\*\fldinst {\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412\charrsid9130272  HYPERLINK "mailto:igor.vlahovic@hgi-cgs.hr" }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid7039412\charrsid9130272 
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the Rizvanu\'9a}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290 a locality, Velebit Mt.}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3153967  (SW Croatia)}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290 ,}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3153967  in order}{
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\ltrch\fcs0 \insrsid6901290 n/Triassic boundary. Continuous Permian/Triassic transitional beds in this area are mainly }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3153967 represented}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290  by ear}{\rtlch\fcs1 \af0 
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\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290 . The}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3153967  most abundant}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290  fossils }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid10249564 
found within early-diagenetic dolomites}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid6901290\charrsid9726473  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid10249564 are }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid6901290\charrsid9726473 
calcareous algae, foraminifera, calcisponges, bryo}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid3153967 zoans, brachiopods and mollusks. }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid14639880 The d}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid6901290 rastic }{
\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid6901290\charrsid9726473 impoverishment of }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid3153967 biota in the uppermost }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid6901290\charrsid9726473 
Permian is associated with a negative excursion at the transition of the }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f3\insrsid6901290\charrsid9726473 \'64}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\super\insrsid6901290\charrsid9726473 13}{\rtlch\fcs1 \af0 \ltrch\fcs0 
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\insrsid6901290\charrsid9726473 0.8 to +2\'89, average +1.2\'b10.5\'89; T: }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 1.3 to +0.9\'89, 0.0\'b10.5\'89), kerogen by up to }{
\rtlch\fcs1 \af0 \ltrch\fcs0 \f37\insrsid6901290\charrsid9726473 5}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 \'89 (P: }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\insrsid6901290\charrsid9726473 27.3 to }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 24.4\'89, }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{\rtlch\fcs1 \af0 
\ltrch\fcs0 \insrsid6901290\charrsid9726473 25.8\'b10.9\'89; T: }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 29.1 to }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{
\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 26.4\'89, }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 27.5\'b10.4\'89). The decrease in the }{\rtlch\fcs1 \af0 
\ltrch\fcs0 \f3\insrsid6901290\charrsid9726473 \'64}{\rtlch\fcs1 \af0 \ltrch\fcs0 \super\insrsid6901290\charrsid9726473 13}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 C values in the carbonates and kerogens }{\rtlch\fcs1 \af0 
\ltrch\fcs0 \insrsid3153967 is}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473  synchronized with a drop in }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 {\field{\*\fldinst SYMBOL 68 \\f "Symbol" \\s 12}{\fldrslt\f3\fs24}}}{
\rtlch\fcs1 \af0 \ltrch\fcs0 \super\insrsid6901290\charrsid9726473 13}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 C}{\rtlch\fcs1 \af0 \ltrch\fcs0 \sub\insrsid6901290\charrsid9726473 carb-ker}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\insrsid6901290\charrsid9726473  by 2\'89, indicating lower productivity at the P/Tr transition.}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 The }{\rtlch\fcs1 \af0 \ltrch\fcs0 
\f3\insrsid6901290\charrsid9726473 \'64}{\rtlch\fcs1 \af0 \ltrch\fcs0 \super\insrsid6901290\charrsid9726473 15}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 N}{\rtlch\fcs1 \af0 \ltrch\fcs0 \sub\insrsid6901290\charrsid9726473 ker}{
\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473  values vary between }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 2.4 to +8.2\'89 (P: +3.7\'b12.8\'89; T: +3.8\'b12.0
\'89), suggesting mixed contribution of }{\rtlch\fcs1 \af0 \ltrch\fcs0 \super\insrsid6901290\charrsid9726473 15}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 N-rich marine (~7\'89) and }{\rtlch\fcs1 \af0 \ltrch\fcs0 
\super\insrsid6901290\charrsid9726473 15}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid9726473 N-depleted terrestrial (~0\'89) organic materials or cyanobacteria (}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid8869314 \u8722\'2d}{\rtlch\fcs1 \af0 
\ltrch\fcs0 \insrsid6901290\charrsid9726473 2 to +4\'89).}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290  
\par }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 REE concentrations in the Upper Permian rocks show a range from 3.7 to 82.4 ppm (average 18.54 }{\rtlch\fcs1 \af174 \ltrch\fcs0 \f174\insrsid11342712 \'b5}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\f174\insrsid11342712 g/g}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 ), while the Lower Triassic dolomites have }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid2304066\charrsid2304066 noticeable}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 
 lower values with range from 8.}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid3687735 7 to 15.4 ppm (average 11.21 }{\rtlch\fcs1 \af174 \ltrch\fcs0 \f174\insrsid3687735 \'b5}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid3687735 g/g}{\rtlch\fcs1 \af0 
\ltrch\fcs0 \f174\insrsid6901290 ). }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290\charrsid9726473 In the uppermost Permian rocks}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 , }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid2239780 approximately }
{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 {\*\xmlopen\xmlns1{\factoidname metricconverter}{\xmlattr\xmlattrns0{\xmlattrname ProductID}{\xmlattrvalue 10 m}}}10 m}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid2239780 {\*\xmlclose} below}{\rtlch\fcs1 
\af0 \ltrch\fcs0 \f174\insrsid6901290  the boundary,}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290\charrsid9726473  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid2239780 there is}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290\charrsid9726473 
 enrichment in most REE}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 . This enrichment is }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290\charrsid9726473 associated with a negative Ce anomaly (1.1 to 0.5)}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\f174\insrsid6901290 , suggesting increased oxidizing conditions in }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid2239780 Late}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 
 Permian sea water and more anoxic conditions towards the boundary (increasing values of Ce/Ce*)}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290\charrsid9726473 .}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290  }{\rtlch\fcs1 \af0 \ltrch\fcs0 
\f174\insrsid3687735 The highest }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 REE concentrations }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid3687735 at}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290  the immediate boundary, with }{\rtlch\fcs1 
\af0 \ltrch\fcs0 \f174\insrsid2239780 both }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290 positive (La, Ce, Pr, Nd, Sm, Eu, Gd, Tm, Lu) and negative (Tb, Dy, Ho, Er, Yb) shifts of the REE}{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid2363868 ,}{
\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid3687735  parallel the positive shift of REE concentrations described in the Idrijca Valley section in Slovenia (}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3687735 Dolenec et al., 2001)}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\f174\insrsid6901290 . }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid3687735 
\par }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 At the boundary there is a substantial decrease in redox sensitive elements}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096  (}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\f174\insrsid14182096\charrsid14182096 2}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 {\field{\*\fldinst SYMBOL 109 \\f "Symbol" \\s 12}{\fldrslt\f3\fs24}}}{\rtlch\fcs1 
\af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 g/g V, }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid14182096 4}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 
{\field{\*\fldinst SYMBOL 109 \\f "Symbol" \\s 12}{\fldrslt\f3\fs24}}}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 g/g }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid14182096\charrsid14182096 U}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\insrsid14182096\charrsid14182096 , and }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid14182096 4}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 {\field{\*\fldinst SYMBOL
 109 \\f "Symbol" \\s 12}{\fldrslt\f3\fs24}}}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 g/g }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid14182096\charrsid14182096 Cr}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 )}{
\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3687735 ,}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid14182096  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 which }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3153967 coincides}{\rtlch\fcs1 
\af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096  with}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096  the maximum of the }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid2239780 Late}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096  Permia}{\rtlch\fcs1 \af0 
\ltrch\fcs0 \insrsid14182096\charrsid14182096 n marine regression}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid12654353 . T}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 he higher concentrations after that event (up to }{\rtlch\fcs1 \af0 
\ltrch\fcs0 \f174\insrsid14182096\charrsid14182096 25}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 {\field{\*\fldinst SYMBOL 109 \\f "Symbol" \\s 12}{\fldrslt\f3\fs24}}}{
\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 g/g V, }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid14182096\charrsid14182096 6}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096  }{\rtlch\fcs1 \af0 \ltrch\fcs0 
\insrsid14182096\charrsid14182096 {\field{\*\fldinst SYMBOL 109 \\f "Symbol" \\s 12}{\fldrslt\f3\fs24}}}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 g/g }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid14182096\charrsid14182096 U}{
\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 , and }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid14182096\charrsid14182096 23}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096  }{\rtlch\fcs1 \af0 \ltrch\fcs0 
\insrsid14182096\charrsid14182096 {\field{\*\fldinst SYMBOL 109 \\f "Symbol" \\s 12}{\fldrslt\f3\fs24}}}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 g/g }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid14182096\charrsid14182096 Cr}{
\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 ) probably indicate the chang}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid12654353 e in redox conditions in Early T}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid14182096\charrsid14182096 
riassic, which again led to oxygen deficiency.}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid12654353  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \f174\insrsid6901290\charrsid14182096 
\par }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098 The variations in the distribution of }{\rtlch\fcs1 \af0 \ltrch\fcs0 \i\insrsid6901290\charrsid3687735 n}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098 -alkanes (C}{\rtlch\fcs1 
\af0 \ltrch\fcs0 \sub\insrsid6901290\charrsid12463276 13}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098  to C}{\rtlch\fcs1 \af0 \ltrch\fcs0 \sub\insrsid6901290\charrsid12463276 34}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\insrsid6901290\charrsid4404098 ), acyclic isoprenoids (C}{\rtlch\fcs1 \af0 \ltrch\fcs0 \sub\insrsid6901290\charrsid12463276 21}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098  to C}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\sub\insrsid6901290\charrsid12463276 28}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098 ), hopanes and steranes, indicate input of bacterial and algal biomass. The occurrence of }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid2239780 odd long-chain }
{\rtlch\fcs1 \af0 \ltrch\fcs0 \i\insrsid2239780\charrsid3687735 n}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid2239780 -alkanes (maximi}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098 zing at C}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\sub\insrsid6901290\charrsid12463276 26}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098 ) and C}{\rtlch\fcs1 \af0 \ltrch\fcs0 \sub\insrsid6901290\charrsid12463276 39}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098 
 steranes in all samples indicate a contribution of continental material. The first results of compound specific C isotope analyses of alkanes indicate a }{\rtlch\fcs1 \af0 \ltrch\fcs0 \super\insrsid6901290\charrsid12463276 
{\*\xmlopen\xmlns1{\factoidname metricconverter}{\xmlattr\xmlattrns0{\xmlattrname ProductID}{\xmlattrvalue 13C}}}13}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290\charrsid4404098 C{\*\xmlclose} depletion 
towards the boundary, supporting the lowering of primary productivity.
\par }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid6901290 
\par }{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid12996410 
\par }\pard \ltrpar\s20\ql \fi-1134\li1134\ri0\widctlpar\wrapdefault\aspalpha\aspnum\faauto\adjustright\rin0\lin1134\itap0\pararsid3687735 {\rtlch\fcs1 \af0 \ltrch\fcs0 \b\insrsid3687735\charrsid3687735 Reference:}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3687735 
 Dolenec T., Lojen S. and Ramov\'9a A. (}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid12996410 2001}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3687735 ) The Permian\u8722\'2d
Triassic boundary in Western Slovenia (Idrijca Valley section): magnetostratigraphy, stable isotopes, and elemental variations. }{\rtlch\fcs1 \af0 \ltrch\fcs0 \i\insrsid3687735\charrsid3687735 Chemical Geology}{\rtlch\fcs1 \af0 \ltrch\fcs0 
\insrsid3687735  }{\rtlch\fcs1 \af0 \ltrch\fcs0 \b\insrsid3687735\charrsid3687735 175}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid3687735 , 175-190.}{\rtlch\fcs1 \af0 \ltrch\fcs0 \insrsid12996410 
\par }}