Palynological Investigation of the Holocene Asahi Submerged Forest in Toyama Prefecture, Central Japan : Palynological Invesigations on the Quaternary System in Japan (2)
著者 Fuji Norio
journal or
publication title
金沢大学教育学部紀要 自然科学編 = Bulletin of the Faculty of Education, Kanazawa University.
Natural science
volume 21
page range 93‑108
year 1972‑12‑15
URL http://hdl.handle.net/2297/22319
9３
PalynologicallnvestigationoftheHoloceneAsahiSubmerged
ForestinToyamaPrefecture，CentralJapan＊－PalynologicallnvestigationsontheQuaternarySysteminJapan(2)－
ＮｏｒｉｏＦＵＪＩ＊＊
lntroduclmn
TheAsahisubmergedforestissituaｔｅｄｉｎｔｈｅｎｏｒｔｈｅｒｎｐａｒｔｏｆＴｏｙａｍａＰｒefecture，
CentralJapanTheforestwasdiscoveredfirstbyShojiFuJエエｏｆｔｈｅＴｏｙａｍａ Ｕｎｉｖｅｒｓｉｔｙｉｎａｂｏｕｔｌ９63．Ｔｈｅｆｏｒｅｓｔｉｓｒｅｃｅｎｔｌｙｆａｍｏｕｓｆｏｒａｇoodevidenceshowing thesubsidenceofgroundtogetherwiththeUozusubmergedforesｔ（FuJｴ,1971)．
Ｔｈｅｐｒｅｓｅｎｔｒｅｐｏｒｔｉｓｔｈｅｓｅｃｏｎｄｏｆｔheseries，‘`RZJylzo〃gicaノＩ)zひCsﾒｶﾞ，α〃o"ｓｏ〃メルｅ Ｑ"α彫γ”γySys2B”′〃JZZPα"，,､Thescopeofthisarticlepaperisthedeterminationof theageofthisforest，palaeoclirnaticconditlonunderwhichtheforestwasgrowingup andgeographicalenvironmentfromtheＶｉｅWpointofpalynologicalinvestigation．
Acknowledgements
HerethewriterwishestorecordhissincerethankstoDr・ShojiFuJIIofthe ToyamaUniveｒｓｉｔｙｆｏｒｈｉｓｋｉｎｄａｄｖｉｃｅｓａｍｐｌｉｎｇｆorthepalynologicalstudyand informationonthestratigraphyoftheAsahisubmergedforest，ａｎｄａｌｓｏｔｏＤｒ、Professor TsuneoXIsHIMAofthelnstituteofWood，KyotoUniversityfortheidentificationof somefossilerectsturnps・ThewriterexpresseshisappreciatｉｏｎｔｏｔｈｅＭｉｎｉｓｔｒｙｏｆ ＥｄｕｃａｔｉｏｎｏｆＪapaneseGovernrnentforsupportfrorntheScienceExpenditureFunds．
GeologicalDescriptionandRe8ultof14Cd2UtingofErectStumpB
TheAsahisubrnergedforestissituatedatDaiya，ＡｓａｈｉＴｏｗｎｉｎｔｈｅｎｏｒｔｈｅｒｎ ｐａｒｔｏｆＴｏyarnaplaininToyarnaPrefecture・TheAsahidistrictoccupiesthenorthern marginoftheKurobefan，andischaracterizedbythes"5"z”，ccガｆｏｒｅｓｔａｎｄａｎｅｒｏｓｉｏｎ ｏｆｔｈｅｃｏａｓｔｏｆJapanＳｅａ
ｌｎｔｈｅＡｓａｈｉｄｉｓｔｒｉｃｔｔｈｅｒｅｉｓasmallcoastalsanddunewhichseemｓｔｏｂｅｆｏｒｍｅｄ ｉｎｔｈｅｌａｔｅｓｔｓｔａｇｅｏｆＹａｙｏｉａｎａｇｅｏｒｔｈｅｅａｒｌｙｓｔａｇｅｏｆＯ１ｄｔｕｍｂａｇｅ，about1,500 yearsbeforethepresent・ThemarginalsedimentoftheKurobeｆａｎｈａｓｂｅｅｎｅｒｏｄｅｄｂｙ ｗａｖｅｓｙｅａｒａｆｔeryear・ＴｈｅｓｕｂｍｅｒｇｅｎｃｅｏｆｔｈｅｃｏａｓｔｉｓｎｏｔｏnlyfoundattheAsahi district，ｂutalsowidelyinthecoastalareasofToyamaPrefecture・Thephenomenon hasbeencontinuingｆｏｒｙｅａｒｓａｎｄｔｈｉｓｉｓｖｅｒｉｆｉｅｄｂｙｔｈｅresultsofthelevelingsurvey，
＊ReceivedSeptember7，1972；theContributionfromthelnstituteofEarthScience，Facultyof Education，KanazawaUniversity，NewSeriesNo､２９；ｒｅａｄＪｕｎｅ２０，１９６５，atthe90thMeetingofthe PalaeontologicalSocietyofJapanheldatKanazawaUniversity．
*＊InstituteofEarthScience,ＦａｃｕｌｔｙｏｆＥｄｕcation,KanazawaUniversity．
第21号昭和47年 9４金沢大学教育学部紀要
andparticularlybytheexistenceofsomesubmergedforests、
Thedistributionofthesubmergedforestisaremarkablecharacterinthecoastal areasofToyamaPrefecturetogetherwithasubmarinecanyon、
ThestudiedareaextendsaboutlOkmｉｎｌｅｎｇｔｈｆｒｏｍｅａｓｔｔｏｗｅｓｔａｎｄ５ｋｍｉｎ width，andcoversalmost５０ｓｑｋｍ・
ＩｎｔｈｅＸｕｒｏｂｅｆａｎｔｈｅｒｅａｒｅｓｏｍｅｂｏｒｉngdata，judgingfromtheseboringdatathe
dｅｐｏｓｉｔｓａｔａｄｅｐｔｈｏｆ４０ｍｅｔｅｒｓｔｏ３０ｍetersbelowthepresentsealevelsuggestthat theymighthavebeensediｍｅｎｔｅｄｉｎｔｈｅｅａｒｌｙｓｔａｇｅｏｆｔｈｅＨｏｌｏcenetransgressionwhich isusuallｙｎａｍｅｄａｓ１ＶｂｏＺ〃"Ｚｃノγα,､soγesszo〃ｏｒ〃α"Cfγ'α〃ノァα,zs9γesszo"．Thesedeposits
●ａｒｅｃｏｍｐｏｓｅｄｏｆｓａｎｄｙｃｌａｙｏｒｍｕｄｄｙｓandandoverliethegravellayerwhichindicates
thelowsealevelduringtheWiirmglacialstage、ThedepositsduringtheHolocene majortransgressionarefoundbetwee、about40or30metersbelowthepresent sealevelandabout5metersabovethe presentsealevel，andaretracedwidely intheKurobefanarea，thissuggests thattheareahadbeensubmergedafter thetimeoftheHolocenemajortransg‐
ressionThesedimentsoftheKurobe fanaremainlycomposedofgravel，thin sandandclaylayers，andcoverthe marinesedimentsbeloｎｇｉｎｇｔｏｔｈｅｔｉｍｅ ｏｆｔｈｅＦ１ａｎｄｒｉａｎｔｒansgression・
Thesubmergedforestshavebeen foundfromsomelocalitiesalongthe coastofToyamaBaysinceadiscovery oftheUozusubmergedforest・The Asahisubmergedforestyieldedｓｏｍｅ ｅｒｅｃｔｓｔｕｍｐｓｏｆｗｏodwhichhavebeen identifiedasfollows：
Ｗ
`祷蕎≦
】
ll1lillF篝illi鑿iiiii
、】露
鰯 Cij》
identitiedas10110ws：
Fig.１．Indexmapshowingthelocalityofthe
samplesfromDaiya,AsahiＴｏｗｎ,Ｔｏｙａｍａ ＡＪ""ｓ〃γs#αTiiRsTAvar．ｓ'鹿γjcdz
Prefecture,CentralJapan． Ａ、ノUZPo"伽ＳＴＥｕＤ Ｘ：Samplinglocality
C〃P‘""ｓｓｐ・
Ｚｂ晩ｏＤａｓｅγγαZaMAKINo
Cγjlｶﾒo”eγ'αノcZPo噸ｏａＤ､ＤＣ頂
Theseerectstumpslaybetweeｎ１．０ｍｅｔｅｒａｎｄ２．Ometersabovethepresentsea
level・Ａｍｏｎｇｔｈｅｍａｂｏｕｔ３０ｐｅｒｃｅｎｔｏｆｔｈｅｅｒｅｃｔｓｔｕｍｐｓｂｅｌｏｎｇｔｏＣγ〃fo"z”ｚａ
ｊ”o"ｊｃｚＺＤ､DON，ａｎｄＡＪ""ｓノヒZPo"′caSmuDoccupiesaboutl5percent・ＡＪ""ｓＦＵＪＩ：PalynologicallnvestigationoftheHoloceneAsahiSubmergedForest 9５
”PC噸ｃｚｚＳＴＥｕＤｇｒｏｗｓｎｅａｒａｓｗａｍｐｙａｒｅａ ａｔthepresent，ａｎｄＣγ〃ﾒo”eγjαノ〃o"ｊｃａ Ｄ・DoNgrowsinplacesnotexposeddirectly totheseabreeze・Thepresentlocationin wheresomeerectstumpswerefoundisthe strandｌｉｎｅｏｆＴｏｙａｍａＢａｙ、
Thestumpsaredistributedinthearea measuring300metersinlengthalonｇｔｈｅ ｃｏａｓｔａｌｌｉｎｅｏｆＤａｉｙａｉｎＡｓａｈｉＴｏｗｎ・In thisareaageologicalunitisclassifiedinto
cobble，coarse-grainedsand，ｃｌａｙ，thickpeat，prese"tｓｅａ＿/eUel fine-grainedsandwithpotterieswhich
〃ﾉＷｅｓＱ"。
/inesQnd妙jｵﾉbpotZeblofｃｌａｙ JqteYbgoijDe7jｏｄ ｐｅｅ２
ｃｌａｙ ｐｅａｔ ｃｏｑ７ｓｅｓα〃d
co66に
■■■■■
●■●●●●■■■
鍔811?；：
ｂｅｌｏｎｇｔｏｔｈｅＯｌｄｔｏｍｂａｇｅ，clayandwhiteFig､２．ColumnarsectionattheLocalityNo・l26
ofDaiya，AsahiＴｏｗｎ，ToyamaPrefect- sanddepositsinascendingorder･Ｔｈｅ
ｕｒｅ,CentralJapan
coarse-grainedsandincorporatestwolayers ofthinpeatanderectstumps・The
fine-grainedsandlayeroccupieｓｂｅｔｗeenlmeterand2metersabovethepresentsea levelatthestrandline・
ThetreesofthoseerectstumpsgrewinthisareaaftertheFlandriantransgression andbeforetheOldtombperiod・Thepeatlayersanalysedinthepresentinvestigation areclassifiedintothinpeatlayerwithcoarse-grainedsandandthickerpeatlayerwhich coverstheclaylayerinascendingorder・
ＡｓａｍｐｌｅｆｒｏｍｔｈｅｅｒｅｃｔｓｔｕｍｐｓｆｏｕｎｄintheAsahisubmergedforestwasdaｔｅｄｂｙ Ｄｒ・KunihikoKIGosmoftheGakushuinUniversity，ａｎｄｔｈｅｒｅｓｕｌｔｏｆ１４Ｃｄａｔｉｎｇｉｓａｓ
ｆｏllows：
ＣｏｄｅＮｏ．GaK-540；apeaceoftheerecttreestump,ＣγjlPjo”eγjαノ6Z'0噸czzD、DoN foundfromonelocality，oftheAsahisubmergedforest36｡57.4′ｉｎＮＬａｔ.，137.34′ｉｎ Ｅ，Long.，alongthecoastline，Daiya，AsahiＴｏｗｎ，ToyamaPrefecture；samplingby ShojiFuJIｴ；1,560±１１０yearsbeforeA．Ｄ、1950.
PalynologicalDegcription
Todothepresentpalynologicalinvestigationl4samples，aUsamplesarepeat lithologically，froml41ocalitiesofDaiya，AsahiTownwereanalysed・Theassemblages ofthepollengrainｓａｎｄｓｐｏｒｅｓｆｏｕｎｄａｒｅｓｈｏｗｎｉｎｔｈｅｐｏllendiagram・Amongthose microfossils，Ｃγ”to”eγiα,Ａ伽"s,Ｔγ'００IPOγαZepollengen、indet・andPjJzSPoγe〃are abundant,ｒａｎｇｉｎｇｆｒｏｍ６ｔｏ２０ｐｅｒｃｅｎｔ、Ｃａ”ｊ""s，〃9Ｊα’０s，Ｐ'eγoczzγyα，Ｆｔｚ９Ｗｓａｎｄ Ｒﾉｸ"ｓａｒｅｃｏｍｍｏｎ，ｓｈｏｗｉｎｇａｆｒｅｑｕｅｎｃｙｏｆ４ｔｏ５ｐｅｒｃｅｎｔ，ａｎｄｔｈｅｏｔｈｅｒｇｅｎｅｒａａｒｅ
第21号昭和47年 9６金沢大学教育学部紀要
rare.ｃγ”'0池”jaisabundant,２１percent ofthetotal，especiallyinthisarea．
Cγ〃わ…ｿﾞﾉα，Ｑ"eγcz`ｓａｎｄＰ‘たSPOγe〃are abundant，andaphenomenonthatthose generaareabundantissupportedbythe erecttreestumpsfromtheAsahiforest・
Theerecttreestumrsareidentifieｄｔｏｂｅ
Ａ腕妬”p018iczZ，Ｃａ”‘""ssp.，ＡＪ"z`ｓ 腕γs#αTuRsTAvar・駆鹿γ'CCZ，Ｚｂﾉﾉbozﾉa sBγγαｊａａｎｄＣγjlPZo”cγ`αノcZPo"jczz・
Amongtheseerectstumps，ＣγjlPｵ0110cγza jZZp0”czZoccupiesabout30percentand A吻妬ノZZp0"iczZaboutl5percent・Eveｎ ｔｈｅｐｌａｎｔｓｗｈｉｃｈｄｏｎｏｔｒｅｍａｉｎａｓ
ＰｉＥＰｃ Ａ６ｉｃｓ ＬＱｒ砿 Ｃ７ｙＰｔｏｍｅｒｍ Ｃｐｃａｓ Ａｌ１ｗ８ ＵｌｍＵ８ My7iopAy〃ｕｍ ＺｅｌＡＯｍｚ ＣｎｒＰｉｎｕＳ Ｃｏ”lu8 Tilia Ju月１０几s PterOcC7Um Fb“ｓＧｅｒ“ium Jle工 Nymphaeaceae Acer E｢icaceae Slzliエ ノVupAc7
〃eDwmMAes Sapotaceae MqJmoljα jWhms RAanwls Que7ctJ8
〃edera TricoIporatepolIen ＰＯＩに〃iCcscf.【＠ＧsⅦｓＲ･Pot･
ＰＤＩ化nｉｌｅｓｃｆｇｅ､皿jntJsR・Pot･
Pollenitesgen､indetsp･a Pollengenindet、
Pollenile8cf･ＥｄｍＩｍｄｆＲ､Pot･
MonosuIcatepollen Meh｢zelligePilzsporen ZweizelligePilzsporen
:;鵬.f説）.)9.,.indel．
20％１０
UollemDiagram（Asahi,locaIityn0.125）
fossilwoodsmaybeidentifiedbytheir
AFi9.3．Diagramshowingtherelationshipbetween fossilpollengrainsorspores，
fossilpollengrainsandsporesfromthe Palynologicalinvestigation，therefore，HolocenedepositsfromDaiya,AsahiTown，
ToyamaPrefecture,CentralJapan、
isimportantfortheinterpretationofthe
ancientflora・Judgingfromtheerecttreestumpsandpollenanalysis，Ｃγ”ﾉo"”jα ﾉﾋZPo"ｊczZmighthavebeenadominantplant、ＡｓＡＪ""ｓノ〃０噸czz，〃９Ｊα,ｚｓａｎｄ Ｑ〃２０””jαノZZPo"ｊｃｚｚｓｈowahighfrequency，ｔｈｅｅｎｖｉｒｏｎｍｅｎｔｍａｙｈａｖｅｂｅｅｎ ａｓｗａｍpyorriparianlowlandnotexposedtoaseabreeze，becausegenusCγjlPﾉo””ja growsgenerallyinanareanotexｐｏｓｅｔｏａｓｅａｂｒｅｅｚｅａｔｔｈｅｐｒｅｓｅｎｔｔｉｍｅ・Ｔｈｅｆｏｒｅｓｔ ｏｆＱ〃ﾒo””zamaybeconsideredtobeanalogoustothosefoundinthetemperate regiｏｎｏｆＪapaneseIslands．
ConcluBion
TheresultofthepalynologicalinvestigationabouttheAsahisubmergedforestis
summarizedasfollows：
（１）ＴｈｅａｇｅｏｆｆｏｒｍａｔｉｏｎｏｆｔｈｅＡｓａｈｉｆｏｒｅｓｔｓｅｅｍｓｔｏｂｅｔｈｅｌａｔｅｓｔＹａｙｏｉｏｒ ｅａrliestO1dtumbperiod，about1,600ｏｒ１，５００yearsbeforethepresent．
（２）ＴｈｅａｇｅｉｎｗｈｅｎｍａｎｙｔｒｅｅｓｆｏｒｌｎｉｎｇｔheAsahiforestweregrowingup,ｉｎ ｔｈｉｓａｒｅａｓｅｅｍｓｔｏｂｅａｂｏｕｔ４,Ｏ００ｔｏａｂｏｕｔｌ,５００yearsbeforethepresentfromthe viewpointofthepalynologicalandgeologicalinvestigationsonthepeatlayersand somecoastalsanddunes，ａｎｄａｌｓｏｔｈｅｒｅｓｕｌｔｏｆ１４Ｃｄａｔｉｎｇｏｆthesubmergederecttree stumps．
（３）Ｔｈｅｃａｕｓｅｏｆｆｏｒｍationofthesubmergedforestisdueｔｏｔｈｅｒｉｓｉｎｇｏｆｓｅａ
ＦｕＪＩ：PalynologicallnvestigationoftheHoloceneAsahiSubmergedForest 9７
Ievelratherthanthesinkingofground・Therisingofsealevel，mmortransgression narnedasYtzyoiα〃ノアα"99'９８s２０"，belongstoafterthelatestYayoiorOldtumbperiod
chronologically，about1,500yearsago．
（４）Thepalaeoclilnaticconditionundｅｒｗｈｉｃｈｔｈｅｔｒｅｅｓｗｅｒｅｇｒｏｗｉｎｇｕｐｂｅfore
theformaｔｉｏｎｏｆｔｈｅｓ"&ﾉﾘz”gecJforestwascoolerthanthatofthepresenttime・Accordingtothewriter,sinvestigation，thecharacteristicplantsarethemixedflora
ofevergreenanddeciduousbroad-1eavedtreesandFzZg"Ｓｃ”"α'αｉｎthecoastalplain ofHOkurikuregion．Ｉｔｉｓａｂｏｕｔｌｏｔｏ２ｏＣ１ｏｗｅｒｔｈaｎｔｈｅｐｒesenttimeinaveragetemperature・Thedecreasingwarmstagemayalmosｔｃｏｒｒｅｓｐｏｎｄｗｉｔｈｔｈｅｔｉｍｅｏｆｔｈｅ
ｍｉｎorfallingofsealevel，ｔｈａｔｉｓ，ｆｐｏｍｔｈｅｍｉｄｄｌｅａｇｅｏｆｔｈｅＴｈｉｒｄＪＯｍｏｎｉａｎｐｅｒｉｏｄｔｏｔｈｅｌａｔｅｓｔａｇｅｏｆｔｈｅＹａｙｏｉａｎｏｒｔｈｅｅａｒｌｉｅｓｔａｇｅｏｆｔｈｅＯｌｄtumbperiod．
ReferencesCited
FuJ1,Ｎ(1965)：PalynologicalStudyontheA11uvialPeatDepositsfromtheHokurikuRegionof
CentralJapan；Ｂ"".Ｆ[zc・ＥＣ！"c､Ｋα"αzα〃αＵ"/".,Nos､１３＆１４．－－－－（1966)：StratigraphicalStudyoftheA11uvialPeatDepositsandBuriedForests；ん"γ・GeoJ．
Ｓｂｃ.'”α",７２，１，
－（1966)：C1imaticChangesofPostglacialAgeinJapan；Ｑ"αf”"αがRCS“伽,5,3.4.
andFuJI1,ｓ.(1967):PostglacialSeaLevelintheJapaneselslands；ん"γ・Geoscj.ＯｓａｈａＣｊｆｙ
[Ｍひ.,10,1-6.
（1971)：PalynologicallnvestigationoftheHoloceneSubmergedForestinToyamaPrefecture，
CentralJapan.-PalynologicallnvestigationsontheQuaternarySysteminJapan(1)-；Ｂ""・
Ftzc．Ｅ伽Cf．Ｋα"czzα〃αＵ"ｉ".，Ｎｏ．２０，NaturalScience，ｐｐ、73-87.
IsHII,I.(1940-41)：OntheRecentMovementoftheStrandLineoftheHokurikuDistrict；ん6地ｅ
Ｐ"6Ｊｊｃａｆｊｏｿｚノ泥沈ｅＣｂﾉﾘ､"zg""γαｆｊｏ〃ｑプProf,ＹＡＢＥ,Ｍ､Ｊ､Ａ，SixtiethBirthday,１１．
第21号昭和47年 9８金沢大学教育学部紀要
ExplanationofPlatel
Fig、１：Ｚｅ鵬“α,polarview,Localityno､124,EKZJ20204・
Fig.２３０α"i""s,polarview,Localityno､129,EKZJ20205・
Fig.３８Ａ！""８，polarview,LocalitynQ126,EKZJ20206、
Fig.４：Ｃｆ.〃0〃"s,polarview,Localityno,128,EKZJ20207、
Ｆｉｇ．５：ＣＯﾌqyJzJs,polarview,Localityno､124,ＥＫZJ20208・
Ｆｉｇ．６：Ａｌ""s,obliquepolarview,Localityno､126,EKZJ20209・
Ｆｉｇ．７：Ｑ””"３，obliquepolarview,Localityno､123,EKZJ20210・
Ｆｉｇ．８：〃〃s,obliquepolarview,Localityno,128,EKZJ20211・
Ｆｉｇ．９：Ｒ"伽３，equatorialview,Localityno､127,EKZJ20212・
Ｆｉｇ．１０：肋9"s,polarview,Localityno､１２7,EKZJ20213・
Ｆｉｇ．１１：Qzsfα"eα,polarview,Localityno､127,EKZJ20214・
Ｆｉｇ．１２：Ｃａｓｆα"eα,polarview,Localityno､127,EKZJ20215、
Ｆｉｇ．１３：FczO秘s，polarview,Localityno､127,EKZJ20216・
Ｆｉｇ．１４：Ｒ幼"s，polarview,LocalitynQ129,EKZJ20217・
Ｆｉｇ．１５：pollengen・indet.,equatorialview,Localiｔｙｎｏ､129,EKZJ20218、
Ｆｉｇ．１６：Ｒ幼"s，polarview,Localityno､127,EKZJ20219・
Ｆｉｇ．１７３Ｐ”sicαγjα,surfaceofgrain,polarview,Localityno､125,EKZJ20220・
Ｆｉｇ．１８：PCJsjc”ｉα,reticulumofgrain,polarview,Localityno､127,EKZJ20221・
Ｆｉｇ．１９．＆２０：PeJsic”ｊα,polarview,LocalityZno､127,ＥＫＪ２０222．
Ｆｉｇ．２１＆22：ｃｃγα"〃”,polarview,Localityno､122,EKZJ20223,surfaceofgrain、
Ｆｉｇ．２３：ｃｃγα"伽加,polarview，equatorialpart,Localityno､122,EKZJ20224・
Ｆｉｇ．248ｓｳﾘ0"“,polarview,Localityno､121,EKZJ20225、
Ｆｉｇ．２５：pollengen・indet.，lateralview，Localityno､121,EKZJ20226．
Ｆis､２６＆27：Fbsso紬”"jczaff.α"､"JCSα,polarview,Localityno､126,EKZJ20227・
Ｆｉｇ．２８：Ｃｆ．Ｓb/αdbpjfys，polａｒｖｉｅｗ，Localityno､129,EKZJ20228．
ＦｕＪＩ：PalynologicallnvestigationoftheHoloceneAsahiSubmergedForestP1.1 9９
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FuJェ：PalynologicallnvestigationoftheHoloceneAsahiSubmergedForest 101
ExplanationofP1atell
Fig、２９：Ｍ`P〃αγ,obliquelateralview,Localityno､121,EKZJ20229・
Fig.３０：ＰＣﾉﾙ"ｉｆｃｓｃｆ・DC"〃""ｓＲ・PoToNIE，equatorialview，Localityno、１２１，EKZJ20230．
’Fig.３１：Ｍｃ〃０７"ﾒｶCs，obliqueequatorialview，Localityno、１２６，EKZJ20231，
Ｆｉｇ．328ＰＣ此"ｊｆｅｓｃｆ.，e"〃""ｓＲ・PoToNIE，equatorialview，Localityno、１２６，EKZJ20232．
’ Ｆｉｇ．338Tricolporatepollen，equatorialview，Localityno、１２１，EKZJ20233・Ｆｉｇ．３４：Fuz9z`s，equatorialview，Localityno，１２３，EKZJ20234・
Ｆｉｇ．３５：Tricolporatepollen，equatorialview，Localityno、１２３，EKZJ20235・
Ｆｉｇ．３６：Ｃｆ・Taxodiaceae，equatorialview，Localityno、１２３，EKZJ20236・
Ｆｉｇ．３７：Ｌαγ灘，equatorialview，Localityno、１２３，EKZJ20237・
Ｆｉｇ．３８：CyCas，polarview，Localityno、１２２，EKZJ20238・
Ｆｉｇ．３９：のcas，polarview，Localityno、１２３
Ｆｉｇ．４０：Sapotaceae，equatorialview，Localityno、１２９，EKZJ20239・
Ｆｉｇ．４１：Cycczs，polarview，Localityno、１２７，EKZJ20240．
Ｆｉｇ．428ＰＣ此"ｉｆｃｓｃｆ・DC""ｉ""ｓＲ・ＰｏＴｏＮＩＥ，equatorialview，Localityno・１２．６’
Ｆｉｇ．４３：Ｃｆ・MdzO"0"α，polarview，Localityno、１２１，EKZJ20241・
Figs、４４＆４５：Ｒ〃"s，equatorialview，Localityno，１２１，EKZJ20242、
Ｆｉｇ．４６：肋021s，equatorialview，Localityno、１２３
Ｆｉｇ．４７：Monosulcateponen，polarview，Localityno、１２９，EKZJ20243、
Ｆｉｇ．４８：Ｃｆ．Ｒ肋,'００`s，equatorialview，Localityno、１２９，EKZJ20244・
Ｆｉｇ．４９：Ａ！"灘s，obliquepolarview，Localityno、１２３，EKZJ20245・
Ｆｉｇ．５０：Ｒ〃"s，equatorialview，Localtyno、１２１，EKZJ20246・
Ｆｉｇ．５１：deciduousQz8e”"s，equatorialview，Localityno、１２２，EKZJ20247-
Figs、５２＆538evergreenＱ"e”２４s，equatorialｖｉｅｗ，Localityno、１２７，ＥＫＺＪ２０２４８ａｎｄＥＫＺＪ
20249.
102金沢大学教育学部紀要 第21号昭和47年
ExplanationofP1atelll
ＧＢγα"伽加，polarview,frontofgrain，Localityno、１２３，EKZJ20250・
ＧＢγα"伽”，polarview，centerofgrain，Loccalityno、１２３，EKZJ20251．
〃“，polarview，Localityno、１２３，EKZJ20252・
Ｃｆ・Nymphaeaceae，polarview，Localityno、１２１，EKZJ20253・
Aceγ，polarview，Localityno、１２１，EKZJ20254、
ＰＣ此"ｉｆｃｓ肋Cs"ｓＲ・PoToNⅡ白polarview，Localityno、１２３，EKZJ20255・
FYz9ws，obliqueequatorialview，Localityno、１２１，EKZJ20256・
Ericaceae，Localityno、１２４，ＥＫＺＪ２０２５７
Ｐｆｃ'0ｃＣＷａ，polarview，Localityno、１２４，EKZJ20258・
Tricolporatepollen，obliqueequatorialview，Localityno、１２９，EKZJ20259・
Ericaceae，Localitｙｎｑｌ２４，EKZJ20260・
Fzz9"s，polarview，Localityno、１２９，ＥＫＺＪ２０２６Ｌ Ｐｆｅγ“α'抑，polarview，Localityno、１３０，EKZJ20262・
Ｃｆ・ひ脇"３，polarview，Localityno、１３０，EKZJ20263・
Ｍｙγｊｑｐ/by"""，polarview，Localityno、１２７，EKZJ20264・
Stzルビ，epuatorialview，Localityno、１２４，EKZJ20265、
Ｑｚ幼蜘"s，polarvieｗ，Localityno、１２２，EKZJ20266・
Tricolporatepollen，polarview，Localityno、１２２，EKZJ20267・
Ｚｅ鵬CDα，obliquepolarview，Localityno、１３０，EKZJ20268、
Tricolporatepollen，polarview，Localityno、１２１，EKZJ20269・
Ｃｆ、Ｐｆ”ocaがα，polarview，Localityno、１２４，EKZJ20270．
●●●●●●●●●●●●●●●●●●●●●〔】□（】（｜（】（一戸】（一（〉（｜（）（一斤墓）｛】（一戸】（一戸】（一一）【｜岸】ロ｜岸）。（〉。｛〉（一声】【一戸〉（一戸】（》岸）（一岸）【一戸》◎一●■■▲●■■仏●ロロュ●□■ら●■ロュ●■■ユ●●■凸●■■△●■■△●■■Ｌ●ご□▲●ロロユ０コ＆●●■△●石口凸●刊冒凸●■■▲●ご■＆●ロ■ａ●■■▲●●□△ＦＦＦＦＦＦＦＦＦＦＦＦＦＦＦＦＦ【肝一ＦＦＦ ●●●●●●●●●●●●●●●●●●●●●●●●●●●●●●●●●●●●。●●●●●●『Ｉ▲ｎ〃］ハペ）４几」一ＦｎＪ〈ｈ）庁Ｊ‐（ｘ）ｎ〕〉〈Ⅱ〉『Ⅱ▲｜ｎ〃】ハペ）４刎乏Ｆ『）（ｈ〉庁Ｊ’ｎｘＵ、】〉（Ⅱ）イー▲『Ⅱユ『Ｉ▲『Ｉ▲イームイーユイー上『Ｉ上『Ｉ▲イー上『Ⅱユーハノ】ｎ〃］
ＦｕＪＩ：PalynologicallnvestigationoftheHoloceneAsahiSubmergedForestPＬＩＩＩ
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ＦｕＪＩ：Palyno1ogicallnvestigationoftheHoloceneAsahiSubmergedForest 105
ExplanationofPlateⅣ Figs、22,23,24,25,26,27＆３１：Ａ/""s，polarview，
Ｆｉｇ．２２：Localityno、１２３，EKZJ20271；Ｆｉｇ．２３：Localityno、１２３，ＥＫＺＪ Ｆｉｇ、２４：Localityno，１２９，EKZJ20273；Ｆｉｇ．２５：Localitynql29,ＥＫＺＪ２０２ Ｆｉｇ、２６：Localityno、１２６，EKZJ20275；Ｆｉｇ．２７：Localitynql24，ＥＫＺＪ２ Ｆｉｇ、３１：Localityno、１２９，EKZJ20277・
Ｆｉｇ．２８：ひ臓"s，polarview，Localityno、１２４，EKZJ20278、
Fig.２９：ＭｙγiqPH1W…，polarview，Localityno，１２４，EKZJ20279、
Fig.３０：Ｚｅ脇oz）α，polarview，Localityno、129．EKZJ20280・
Fig.３２＆３３：OUz幼吻"３，polarview，Localityno、１３０，EKZJ20281，EKZJ20282・
Ｆｉｇ．３４：⑰が！"s，polarview，Localityno、１３０，EKZJ20283・
Ｆｉｇ．３５：Ｔ"zα，polarview，Localityno、１２７，EKZJ20284・
Ｆｉｇ．３６：Tricolpatepollen，polarview，Localityno、１２６，EKZJ20285・
Ｆｉｇ．３７：Ｃｆ・ＴｊＪｊｃｚ，polarview，Localityno、１２６，EKZJ20286・
Ｆｉｇ．３８：CCZ”ｉ""s，polarview，Localityno、１２９，EKZJ20287、
Fig.３９：〃,肱"８，polarview，Localityno、１２７，EKZJ20288・
Fig.４０：〃0〃"s，polarview，Localityno、１２４，EKZJ20289・
Fig.418ＰｆｅγひＣａがα，polarview，Localityno、１２６，EKZJ20290
Figs、４２：＆４３：Ｃｆ．〃O〃"s，polarview，Localityno、１２９，ＥＫＺＪ２０２９１；Localityno・
l28EKZJ20292．
23：Localityno、１２３，EKZJ20272；
25：Localitynql29,EKZJ20274；
27：Localitynql24，EKZJ20276；
第21号昭和47年 106金沢大学教育学部紀要
ExplanationofP1ateV
18PjMz，lateralview，Localityno､121,EKZJ20293、
28Ａ〃９３，１ateralview，Localityno、１２１，EKZJ20294、
3：Ｐ⑰ｄｂｃａ”"s’１ateralview，Localityno、１２３，EKZJ20295 48PjCea，Iateralview・Localityno、１２１，EKZJ20296、
5-198Taxodiaceae（Cf．Ｃ伽/o加”ｉα)，
Figs、６＆１４：centerofgrain，Fig.７：frontofgrain，
Figs、5,6,7＆１３：Localityno・’24,EKZJ20298，20299,Asahi，ToyamaPref.，
●●●●●＆』〕句些。【】。（】。序型。（）つじ一■＆●一■△●■■△ｏ■▲●一■且【凶△【Ｈ《【脚（【一ｍ△【Ｈ《
Fig.８：Localityno、１３０，EKZJ20300；
Figs、９＆l08Localityno、１２６，EKZJ20301、20302；
Figs、１１＆１９：Localityno、１３０，EKZJ20303，20304；
Figs、１２＆188Localityno・l2LEKZJ20305，20306；
Fig.１３：Localityno、１２５，EKZJ20307；
Fig.１４：Localityno、１２８，EKZJ20308；
Figs、１５，１６＆１７：Localityno、１２９，ＥＫＺＪ２０309,20310, 20311.
ExplanationofP1ateⅥ
Figs、20-25：MehrzelligePilzsporen，Ｆｉｇ．208Localityno、123,ＥＫＺＪ２０３１２
Ｆｉｇ、２１：Localityno、１２３，EKZJ20313；Ｆｉｇ．228Localityno、１２９，EKZJ20314；
Ｆｉｇ．２３：Localityno、１２８，EKZJ20315；
Ｆｉｇ．２４：Localityno､128,EKZJ20316；
Ｆｉｇ．２５：Localityno、１２８，EKZJ20317・
Figs、26-28：ZweizelligePilzsporen，Ｆｉｇ．２６：Localityno、１２３，EKZJ20318；
Ｆｉｇ．２７：Localiyno、１２９，EKZJ20319；Ｆｉｇ．２８：Localityno、１２４，EKZJ20320・
Figs、29-328Polypodiaceae，lateralview,Fig.２９：Localityno､123,EKZJ20321；
Ｆｉｇ．３０：Localityno、１２９，EKZJ20322；Ｆｉｇ．318Localitynql29，EKZJ20323；
Ｆｉｇ．３2：Localityno、１２９，EKZJ20324・
Ｆｉｇ．３３：Sporegen･indet.，Localityno、130,ＥＫＺＩ２０３２５・
Ｆｉｇ．３４：Polypodiaceae，１ateralview，Localityno・’30,EKZJ20326・
Ｆｉｇ．３５：Monosulcate，polarview，Localityno、126,EKZJ20327、
Ｆｉｇ．３６：Polypodiaceae，lateralview，Localityno、１２３，EKZJ20328・
Ｆｉｇ．３７：ＰＣlypodiaceae，１ateralview，Localityno、１２９，EKZJ20329・
Ｆｉｇ．388Genusindet・’１ateralview，Localityno、１２９，EKZJ20330、
Ｆｉｇ．398Pollenwithpollen-tube，１ateralview，Localityno、１２９，EKZJ20331・
Ｆｉｇ．４０：CjDIPfo"Ceγiczcf、ノapo"ｉcc７，１ateralview，Localityno、１２９，EKZJ20332．
ＦｕＪＩ：PalynologicallnvestigationoftheHoloceneAsahiSubmergedForest Ｐ1.Ｖ 1０７
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