大量絶滅の引き金になった食物連鎖の崩壊(<特集2>白亜紀末の大量絶滅事変に残る謎)
白亜紀/古第三紀境界の大量絶滅は、地球史の中でも有数規模であった。絶滅は、特に光合成生物とそれを直接的な基盤とする生食連鎖に属する生物について顕著であるのに対し、いわゆる腐食連鎖に属していたと考えられる生物は大きな被害を受けていない。また、石灰質の殻を持つ海洋生物の絶滅率が突出して高いという特徴がある。絶滅を引き起こした原因として、直径10kmの小惑星の地球への衝突が引き金となり、その後に発生した複合的な環境変動が考えられる。具体的には、太陽光の遮断による光合成の停止と寒冷化、酸性雨や有毒物質による陸上・海洋の汚染、そして輻射熱による地表面の高温化などが、大量絶滅パターンを説明できる環境変動と...
Saved in:
| Published in | Nihon Seitai Gakkai shi Vol. 64; no. 1; pp. 39 - 46 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | Japanese |
| Published |
一般社団法人 日本生態学会
2014
The Ecological Society of Japan |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0021-5007 2424-127X |
| DOI | 10.18960/seitai.64.1_39 |
Cover
| Abstract | 白亜紀/古第三紀境界の大量絶滅は、地球史の中でも有数規模であった。絶滅は、特に光合成生物とそれを直接的な基盤とする生食連鎖に属する生物について顕著であるのに対し、いわゆる腐食連鎖に属していたと考えられる生物は大きな被害を受けていない。また、石灰質の殻を持つ海洋生物の絶滅率が突出して高いという特徴がある。絶滅を引き起こした原因として、直径10kmの小惑星の地球への衝突が引き金となり、その後に発生した複合的な環境変動が考えられる。具体的には、太陽光の遮断による光合成の停止と寒冷化、酸性雨や有毒物質による陸上・海洋の汚染、そして輻射熱による地表面の高温化などが、大量絶滅パターンを説明できる環境変動として挙げられる。今後、生態学的研究により、観測されている絶滅パターンを再現するために必要な環境変動の規模や持続時間を解明することが望まれる。 |
|---|---|
| AbstractList | 白亜紀/古第三紀境界の大量絶滅は、地球史の中でも有数規模であった。絶滅は、特に光合成生物とそれを直接的な基盤とする生食連鎖に属する生物について顕著であるのに対し、いわゆる腐食連鎖に属していたと考えられる生物は大きな被害を受けていない。また、石灰質の殻を持つ海洋生物の絶滅率が突出して高いという特徴がある。絶滅を引き起こした原因として、直径10kmの小惑星の地球への衝突が引き金となり、その後に発生した複合的な環境変動が考えられる。具体的には、太陽光の遮断による光合成の停止と寒冷化、酸性雨や有毒物質による陸上・海洋の汚染、そして輻射熱による地表面の高温化などが、大量絶滅パターンを説明できる環境変動として挙げられる。今後、生態学的研究により、観測されている絶滅パターンを再現するために必要な環境変動の規模や持続時間を解明することが望まれる。 |
| Author | 後藤, 和久 |
| Author_FL | Goto Kazuhisa |
| Author_FL_xml | – sequence: 1 fullname: Goto Kazuhisa |
| Author_xml | – sequence: 1 fullname: 後藤, 和久 organization: 東北大学災害科学国際研究所 |
| BackLink | https://cir.nii.ac.jp/crid/1390001204291966464$$DView record in CiNii https://agriknowledge.affrc.go.jp/RN/2010872241$$DView record in AgriKnowledge |
| BookMark | eNpNkU9LG0EYhwex0Gg99wv0oIdN3_mzszNQCiKtrRW8WOhtmN3MphNjoruB0psrqKShlh5aEAUPEUQtnqxQq59mTbb7LbpLRLz83sP7_J7D-06g8Va7ZRB6iqGKheTwPDa2o22VsypWVI6hCmGEOZh4H8ZRBYBgxwXwHqOpOLY-EKCCgIcraH1wdJzvfMt-Xw7_bqXJ-eD6R5p8zXe-p8lZmpymST9NDvP-YdY9yTf6-e7Pkrk4GfS_TL_Iun_y_W3yMtu7ub06yC42hgdn5fqB8faqNzjqFq7heS_d7P37tTvzBD0KdTM2U3dzEr1__Wp57o2zuDT_dm520dGEe8xh3AVP-sCNdv0wrBGhhfClYdgXmhJpsOeFQS0A32WCaSowYa4BIbRhxHc5nUTeyKvDMLIdpeuRXWm1PzVNrW5UW1tVLgJVb6vGmgKsivtQzAEXzWejZstaFdgyMZUAgAkwIrHknHFWYAsjrBF3dKFci-yqjj4rHXVs0DRq9BLFmcJlvFsoDCApES4X91DwUUeqoel_-gqu7Q |
| ContentType | Journal Article |
| Copyright | 2014 一般社団法人 日本生態学会 |
| Copyright_xml | – notice: 2014 一般社団法人 日本生態学会 |
| DBID | RYH N5S |
| DOI | 10.18960/seitai.64.1_39 |
| DatabaseName | CiNii Complete AgriKnowledge（アグリナレッジ）AGROLib |
| DatabaseTitleList | |
| DeliveryMethod | fulltext_linktorsrc |
| Discipline | Ecology |
| DocumentTitleAlternate | Cretaceous/Paleogene mass extinction was triggered by the collapse of the food chain(<Feature 2>Remaining mysteries in the K/Pg mass extinction) |
| DocumentTitle_FL | Cretaceous/Paleogene mass extinction was triggered by the collapse of the food chain(<Feature 2>Remaining mysteries in the K/Pg mass extinction) |
| EISSN | 2424-127X |
| EndPage | 46 |
| ExternalDocumentID | oai_affrc_go_jp_01_00731601 110009810891 article_seitai_64_1_64_KJ00009328568_article_char_ja |
| GroupedDBID | -~X 2WC 5GY ALMA_UNASSIGNED_HOLDINGS JSF OK1 RJT 53G ECGQY RYH N5S |
| ID | FETCH-LOGICAL-a2674-465079b06ea5bffd28a88b9e41b8a329e177fcdc0b5484a381245e088ae42b563 |
| ISSN | 0021-5007 |
| IngestDate | Fri Sep 19 12:23:12 EDT 2025 Fri Jun 27 00:24:27 EDT 2025 Wed Apr 05 05:52:12 EDT 2023 |
| IsDoiOpenAccess | true |
| IsOpenAccess | true |
| IsPeerReviewed | false |
| IsScholarly | true |
| Issue | 1 |
| Language | Japanese |
| LinkModel | OpenURL |
| MergedId | FETCHMERGED-LOGICAL-a2674-465079b06ea5bffd28a88b9e41b8a329e177fcdc0b5484a381245e088ae42b563 |
| Notes | 872241 ZZ00015063 |
| ORCID | 0000-0002-5351-7383 |
| OpenAccessLink | https://agriknowledge.affrc.go.jp/RN/2010872241 |
| PageCount | 8 |
| ParticipantIDs | affrit_agriknowledge_oai_affrc_go_jp_01_00731601 nii_cinii_1390001204291966464 jstage_primary_article_seitai_64_1_64_KJ00009328568_article_char_ja |
| PublicationCentury | 2000 |
| PublicationDate | 2014 |
| PublicationDateYYYYMMDD | 2014-01-01 |
| PublicationDate_xml | – year: 2014 text: 2014 |
| PublicationDecade | 2010 |
| PublicationTitle | Nihon Seitai Gakkai shi |
| PublicationTitleAlternate | 生態誌 |
| PublicationTitle_FL | JAPANESE JOURNAL OF ECOLOGY 生態誌 |
| PublicationYear | 2014 |
| Publisher | 一般社団法人 日本生態学会 The Ecological Society of Japan |
| Publisher_xml | – name: 一般社団法人 日本生態学会 – name: The Ecological Society of Japan |
| References | Belcher CM, Collinson ME, Scott AC (2005) Constraints on theThermal Power Released from the Chicxulub Impactor: NewEvidence from Multi-Method Charcoal Analysis. Journal ofthe Geological Society of London, 162:591-602 MacRae RA, Fensome RA, Williams GL (1996) FossilDinoflagellate diversity, originations, and extinctions andtheir significance. Canadian Journal of Botany, 74:1687-1694 Pope KO (2002) Impact dust not the cause of the Cretaceous-Tertiary mass extinction. Geology 30:99-102 Bown PR, Lees JA, Young JR (2004) Calcareous nannoplanktonevolution and diversity through time. In: Thierstein HR,Young JR (eds), Coccolithophores, From MolecularProcesses to Global Impact, 481-508. Springer, Berlin 大野 宗祐 (2014) 天体衝突が引き起こす環境変動と大量絶滅. 日本生態学会誌, 64:55-62 D’Hondt S, Pilson MEQ, Sigurdsson H, Hanson A, Carey S(1994) Surface-water acidification and extinction at theCretaceous-Tertiary boundary. Geology, 22:983-986 Saito T, Yamanoi T, Kaiho K (1986) End-Cretaceousdevastation of terrestrial flora in the boreal Far East. Nature,323:253-255 Gupta SC, Ahrens TJ, Yang W (2001) Shock-inducedvaporization of anhydrite and global cooling from the K/Timpact. Earth and Planetary Science Letters, 188:399-412 Erickson DJ III, Dickson SM (1987) Global trace elementbiogeochemistry at the K/T boundary: The oceanic andbiotic response to a hypothetical meteorite impact. Geology,15:1014-1017 Harvey M, Brassell SC, Belcher CM, Montanari A, (2008)Combustion of fossil organic matter at the CretaceousPaleogene (K-P) boundary. Geology, 36:355-358 Pospichal JJ (1994) Calcareous nannofossils at the K/Tboundary, El Kef: No evidence for stepwise, gradual orsequential extinctions. Geology, 22:99-102 Kitchell JA, Clark DL, Gombos AM (1986) Biologicalselectivity of extinction: a link between background andmass extinction. Palaios, 1:504-511 Zachos JC, Arthur MA, Dean W (1989) Geochemical evidencefor suppression of marine productivity at the Cretaceous/Tertiary boundary. Nature, 337:61-64 Bown PR (2005) Selective calcareous nannoplanktonsurvivorship at the Cretaceous-Tertiary boundary. Geology,33:653-656 Pope KO, Baines KH, Ocampo AC, Ivanov B (1997) Energy,volatile production, and climatic effects of the ChicxulubCretaceous/Tertiary impact. Journal of Geophysical Research,102:21645-21664 Tschudy RH, Pillmore CL, Orth CJ, Gilmore JS, Knight JD(1984) Disruption of the terrestrial plant ecosystemat theCretaceous-Tertiary boundary, western interior. Science225:1030-1032 Nichols DJ, Johnson KR (2008) Plants and the K-T boundary,Cambridge Univ. Press, United Kingdom 高橋 昭紀, 後藤, 和久 (2010) 恐竜絶滅研究の最前線. 科学,80:945-953 Orth CJ, Gilmore JS, Knight JD, Pillmore CL, Tschudy RH,Fassett JE (1981) An iridium abundance anomaly at thepalynological Cretaceous-Tertiary boundary in northern NewMexico. Science, 214:1341-1343 Surlyk F (1990) Cretaceous-Tertiary (Marine). In Brrigs DEG,Crowther PR (eds), Paleobiology Asynthesis. 198-203.Blackwell Sci. Publ., Oxford Sweet AR, Braman DR (2001) Cretaceous-Tertiary palynofloralperturbations and extinctions with the AquilapollenitesPhytogeographic Province. Canadian Journal of EarthSciences, 38:249-269 Sepúlveda J, Wendler J, Summons RE, Hinrichs K (2009)Rapid resurgence of marine productivity after the cretaceouspaleogenemass extinction. Science, 326:129-132 Wolbach WS, Lewis RS, Anders E (1985) Cretaceousextinctions: evidence for wildfires and search for meteoriticmaterial. Science, 230:167-170 Kring D (2007) The Chicxulub impact event and itsenvironmental consequences at the Cretaceous-Tertiary boundary. Palaeogeography, Palaeoclimatology,Palaeoecology, 255:4-21 D’Hondt S (2005) Consequences of the Cretaceous/Paleogenemass extinction for marine ecosystems. Annual Review ofEcology Evolution and Systematics, 36:295-317 Belcher CM (2009) Reigniting the Cretaceous-PalaeogeneFirestorm Debate. Geology, 37:1147-1148. 平野 弘道 (2006) 絶滅古生物学. 岩波書店, 東京 Sheehan PM, Fastovsky DE (1992) Major extinctions of landdwellingvertebrates at the Cretaceous-Tertiary boundary,eastern Montana. Geology, 20:556-560 Sheehan PM, Coorough PJ, Fastovsky DE (1996) Bioticselectivity during the K/T and Late Ordovician extinctionevents. Geological Society of America Special Paper,307:477-489 Galeotti S, Brinkhuis H, Huber M (2004) Records of post-Cretaceous-Tertiary boundary millennial-scale cooling fromthe western Tethys: A smoking gun for the impact-winterhypothesis? Geology, 32:529-532 Sheehan PM, Hansen TA (1986) Detritus feeding as a buffer toextinction at the end of the Cretaceous. Geology, 14:868-870 Hallam A, Perch-Nielsen K (1990) The biotic record ofevents in the marine realm at the end of the Cretaceous:calcareous, siliceous and organic-walled microfossils andmacroinvertebrates. Tectonophysics, 171:347-357 Toon OB, Zahnle K, Morrison D, Turco RP, Covey C (1997)Environmental perturbations caused by the impacts ofasteroids and comets. Review of Geophysics, 35:41-78 Habib D, Moshkovitz S, Kramer C (1992) Dinoflagellateand calcareous nannofossil response to sea-level change inCretaceous-Tertiary boundary sections. Geology, 20:165-168 Maruoka T, Koeberl C (2003) Acid-neutralizing scenario afterthe Cretaceous-Tertiary impact event. Geology, 31:489-492 Kring DA, Durda DD (2002) Trajectories and distributionof material ejected from the Chicxulub impact crater:Implications for post impact wildfires. Journal of GeophysicalResearch, 107:6-22 Jiang S, Bralower TJ, Patzkowsky ME, Kump LR, SchuethJD (2010) Geographic controls on nannoplankton extinctionacross the Cretaceous/Palaeogene boundary. NatureGeoscience, 3:280-285 Goldin TJ, Melosh HJ (2009) Self-shielding of thermalradiation by Chicxulub impact ejecta: Firestorm or fizzle?Geology, 37:1135-1138 Ohno S, Sugita S, Kadono T, Hasegawa S, Igarashi G (2004)Sulfur chemistry in laser-simulated impact vapor clouds:implications for the K/T impact event. Earth and PlanetaryScience Letters, 218:347-361 Vajda V, McLoughlin S (2004) Fungal Proliferation at theCretaceous-Tertiary Boundary. Science, 303:1489 Wilf P, Johnson KR, Huber BT (2003) Correlated terrestrialand marine evidence for global climate changes beforemass extinction at the Cretaceous-Paleogene boundary.Proceedings of National Academy of Science, 100:599-604 Miya M, Friedman M, Satoh TP, Takeshima H, Sado T, IwasakiW, Yamanoue Y, Nakatani M, Mabuchi K, Inoue JG, PoulsenJY, Fukunaga T, Sato Y, Nishida M (2013) EvolutionaryOrigin of the Scombridae (Tunas and Mackerels): Membersof a Paleogene Adaptive Radiation with 14 Other PelagicFish Families. PLOS ONE, 8:e73535. Belcher CM, Collinson ME, Sweet AR, Hildebrand AR, ScottAC (2003) Fireball Passes and Nothing Burns - The Roleof Thermal Radiation in the K-T Event: Evidence from theCharcoal Record of North America. Geology, 31:1061-1064 Hollis CJ, Rodgers KA, Parker RJ (1995) Siliceous planktonbloom in the earliest Tertiary of Marlborough, New Zealand.Geology, 23:835-838 Pierazzo E, Kring DA, Melosh HJ (1998) Hydrocode simulationof the Chicxulub impact event and the production ofclimatically active gases. Journal of Geophysical Research,103:28607-28625. Hildebrand AR, Penfield GT, Kring DA, Pilkington M, AntonioCZ, Jacobsen SB, Boynton WV (1991) Chicxulub crater: apossible Cretaceous/Tertiary boundary impact crater on theYucatán Peninsula, Mexico. Geology, 19:867-871 Robertson DS, McKenna MC, Toon OB, Hope S, LillegravenJA (2004) Survival in the first hours of the Cenozoic.Geological Society of America Bulletin, 116:760-768 Toon OB, Pollack JP, Ackerman TP, Turco RP, McKay CP, LiuMS (1982) Evolution of an impact generated dust cloud andits effects on the atmosphere. Geological Society of AmericaSpecial Paper, 190:187-200 Cavin I (2001) Effects of the Cretaceous-Tertiary boundaryevent on bony fishes. In: Buffetaut E, Koeberl G (eds),Geological and biological effects of impact events, 141-158.Springer Verlag, Berlin, Germany Adams JB, Mann ME, D’Hondt S (2004) The Cretaceous-Tertiary extinction: Modeling carbon flux and ecologicalresponse. Paleoceanography, 19:PA1002 Alvarez LW, Alvarez W, Asaro F, Michel HV (1980)Extraterrestrial cause for the Cretaceous-Tertiary extinction.Science, 208:1095-1108 D’Hondt S, Donaghay P, Zachos JC, Luttenberg D, LindingerM (1998) Organic Carbon Fluxes and Ecological Recoveryfrom the Cretaceous-Tertiary Mass Extinction. Science,282:276-289 Schulte P, Alegret L, Arenillas I, Arz JA, Barton PJ, Bown PR,Bralower TJ, Christeson GL, Claeys P, Cockell CS, CollinsGS, Deutsch A, Goldin TJ, Goto K, Grajales-Nishimura JM,Grieve RAF, Gulick SPS, Johnson KR, Kiessling W, KoeberlC, Kring DA, MacLeod KG, Matsui T, Melosh J, MontanariA, Morgan JV, Neal CR, Nichols DJ, Norris RD, PierazzoE, Ravizza G, Rebolledo-Vieyra M, Reimold WU, Robin E,Salge T, Speijer RP, Sweet AR, Urrutia-Fucugauchi J, VajdaV, Whalen MT, Willumsen PS (2010) The Chicxulub asteroidimpact and mass extinction at the Cretaceous-PaleogeneBoundary. Science, 327:1214-1218 Pierazzo E, Hahmann AN, Sloan LC (2003) Chicxulub andclimate: radiative perturbations of impact-produced S-bearinggases. Astrobiology, 3:99-118 後藤, 和久 (2011) 決着！恐竜絶滅論争．岩波科学ライブラリー186巻. 岩波書店, 東京 Belcher CM, Finch P, Collinson ME, Scott AC, GrassineauNV (2009) Geochemical Evidence for Combustion ofHydrocarbons During the K-T Impact Event. Proceedings ofthe National Academy of Sciences, 106:4112-4117 Melosh HJ, Schneider NM, Zahnle KJ, Latham D (1990)Ignition of global wildfires at the Cretaceous/Tertiaryboundary. Nature, 343:251-254 Shuvalov VV (2002) Radiation effects of the Chicxulub impactevent. In: Buffetaut E, Koeberl C (eds), Geological andBiological Effects of Impact Events, 237-247. Springer,Berlin Vajda V, Raine JI, Hollis CJ (2001) Indication of globaldeforestation at the Cretaceous-Tertiary boundary by NewZealand fern spike. Science 294:1700-1702 |
| References_xml | – reference: Saito T, Yamanoi T, Kaiho K (1986) End-Cretaceousdevastation of terrestrial flora in the boreal Far East. Nature,323:253-255 – reference: Tschudy RH, Pillmore CL, Orth CJ, Gilmore JS, Knight JD(1984) Disruption of the terrestrial plant ecosystemat theCretaceous-Tertiary boundary, western interior. Science225:1030-1032 – reference: Orth CJ, Gilmore JS, Knight JD, Pillmore CL, Tschudy RH,Fassett JE (1981) An iridium abundance anomaly at thepalynological Cretaceous-Tertiary boundary in northern NewMexico. Science, 214:1341-1343 – reference: Kring D (2007) The Chicxulub impact event and itsenvironmental consequences at the Cretaceous-Tertiary boundary. Palaeogeography, Palaeoclimatology,Palaeoecology, 255:4-21 – reference: 大野 宗祐 (2014) 天体衝突が引き起こす環境変動と大量絶滅. 日本生態学会誌, 64:55-62 – reference: D’Hondt S, Pilson MEQ, Sigurdsson H, Hanson A, Carey S(1994) Surface-water acidification and extinction at theCretaceous-Tertiary boundary. Geology, 22:983-986 – reference: D’Hondt S, Donaghay P, Zachos JC, Luttenberg D, LindingerM (1998) Organic Carbon Fluxes and Ecological Recoveryfrom the Cretaceous-Tertiary Mass Extinction. Science,282:276-289 – reference: Belcher CM, Finch P, Collinson ME, Scott AC, GrassineauNV (2009) Geochemical Evidence for Combustion ofHydrocarbons During the K-T Impact Event. Proceedings ofthe National Academy of Sciences, 106:4112-4117 – reference: 平野 弘道 (2006) 絶滅古生物学. 岩波書店, 東京 – reference: MacRae RA, Fensome RA, Williams GL (1996) FossilDinoflagellate diversity, originations, and extinctions andtheir significance. Canadian Journal of Botany, 74:1687-1694 – reference: Vajda V, McLoughlin S (2004) Fungal Proliferation at theCretaceous-Tertiary Boundary. Science, 303:1489 – reference: Pope KO, Baines KH, Ocampo AC, Ivanov B (1997) Energy,volatile production, and climatic effects of the ChicxulubCretaceous/Tertiary impact. Journal of Geophysical Research,102:21645-21664 – reference: D’Hondt S (2005) Consequences of the Cretaceous/Paleogenemass extinction for marine ecosystems. Annual Review ofEcology Evolution and Systematics, 36:295-317 – reference: Erickson DJ III, Dickson SM (1987) Global trace elementbiogeochemistry at the K/T boundary: The oceanic andbiotic response to a hypothetical meteorite impact. Geology,15:1014-1017 – reference: Maruoka T, Koeberl C (2003) Acid-neutralizing scenario afterthe Cretaceous-Tertiary impact event. Geology, 31:489-492 – reference: Robertson DS, McKenna MC, Toon OB, Hope S, LillegravenJA (2004) Survival in the first hours of the Cenozoic.Geological Society of America Bulletin, 116:760-768 – reference: Toon OB, Zahnle K, Morrison D, Turco RP, Covey C (1997)Environmental perturbations caused by the impacts ofasteroids and comets. Review of Geophysics, 35:41-78 – reference: 後藤, 和久 (2011) 決着！恐竜絶滅論争．岩波科学ライブラリー186巻. 岩波書店, 東京 – reference: Surlyk F (1990) Cretaceous-Tertiary (Marine). In Brrigs DEG,Crowther PR (eds), Paleobiology Asynthesis. 198-203.Blackwell Sci. Publ., Oxford – reference: Schulte P, Alegret L, Arenillas I, Arz JA, Barton PJ, Bown PR,Bralower TJ, Christeson GL, Claeys P, Cockell CS, CollinsGS, Deutsch A, Goldin TJ, Goto K, Grajales-Nishimura JM,Grieve RAF, Gulick SPS, Johnson KR, Kiessling W, KoeberlC, Kring DA, MacLeod KG, Matsui T, Melosh J, MontanariA, Morgan JV, Neal CR, Nichols DJ, Norris RD, PierazzoE, Ravizza G, Rebolledo-Vieyra M, Reimold WU, Robin E,Salge T, Speijer RP, Sweet AR, Urrutia-Fucugauchi J, VajdaV, Whalen MT, Willumsen PS (2010) The Chicxulub asteroidimpact and mass extinction at the Cretaceous-PaleogeneBoundary. Science, 327:1214-1218 – reference: Belcher CM, Collinson ME, Scott AC (2005) Constraints on theThermal Power Released from the Chicxulub Impactor: NewEvidence from Multi-Method Charcoal Analysis. Journal ofthe Geological Society of London, 162:591-602 – reference: Jiang S, Bralower TJ, Patzkowsky ME, Kump LR, SchuethJD (2010) Geographic controls on nannoplankton extinctionacross the Cretaceous/Palaeogene boundary. NatureGeoscience, 3:280-285 – reference: Gupta SC, Ahrens TJ, Yang W (2001) Shock-inducedvaporization of anhydrite and global cooling from the K/Timpact. Earth and Planetary Science Letters, 188:399-412 – reference: Habib D, Moshkovitz S, Kramer C (1992) Dinoflagellateand calcareous nannofossil response to sea-level change inCretaceous-Tertiary boundary sections. Geology, 20:165-168 – reference: Toon OB, Pollack JP, Ackerman TP, Turco RP, McKay CP, LiuMS (1982) Evolution of an impact generated dust cloud andits effects on the atmosphere. Geological Society of AmericaSpecial Paper, 190:187-200 – reference: Sheehan PM, Coorough PJ, Fastovsky DE (1996) Bioticselectivity during the K/T and Late Ordovician extinctionevents. Geological Society of America Special Paper,307:477-489 – reference: Cavin I (2001) Effects of the Cretaceous-Tertiary boundaryevent on bony fishes. In: Buffetaut E, Koeberl G (eds),Geological and biological effects of impact events, 141-158.Springer Verlag, Berlin, Germany – reference: Hildebrand AR, Penfield GT, Kring DA, Pilkington M, AntonioCZ, Jacobsen SB, Boynton WV (1991) Chicxulub crater: apossible Cretaceous/Tertiary boundary impact crater on theYucatán Peninsula, Mexico. Geology, 19:867-871 – reference: Kitchell JA, Clark DL, Gombos AM (1986) Biologicalselectivity of extinction: a link between background andmass extinction. Palaios, 1:504-511 – reference: Pospichal JJ (1994) Calcareous nannofossils at the K/Tboundary, El Kef: No evidence for stepwise, gradual orsequential extinctions. Geology, 22:99-102 – reference: Wolbach WS, Lewis RS, Anders E (1985) Cretaceousextinctions: evidence for wildfires and search for meteoriticmaterial. Science, 230:167-170 – reference: Bown PR, Lees JA, Young JR (2004) Calcareous nannoplanktonevolution and diversity through time. In: Thierstein HR,Young JR (eds), Coccolithophores, From MolecularProcesses to Global Impact, 481-508. Springer, Berlin – reference: Sepúlveda J, Wendler J, Summons RE, Hinrichs K (2009)Rapid resurgence of marine productivity after the cretaceouspaleogenemass extinction. Science, 326:129-132 – reference: Alvarez LW, Alvarez W, Asaro F, Michel HV (1980)Extraterrestrial cause for the Cretaceous-Tertiary extinction.Science, 208:1095-1108 – reference: Galeotti S, Brinkhuis H, Huber M (2004) Records of post-Cretaceous-Tertiary boundary millennial-scale cooling fromthe western Tethys: A smoking gun for the impact-winterhypothesis? Geology, 32:529-532 – reference: Ohno S, Sugita S, Kadono T, Hasegawa S, Igarashi G (2004)Sulfur chemistry in laser-simulated impact vapor clouds:implications for the K/T impact event. Earth and PlanetaryScience Letters, 218:347-361 – reference: Shuvalov VV (2002) Radiation effects of the Chicxulub impactevent. In: Buffetaut E, Koeberl C (eds), Geological andBiological Effects of Impact Events, 237-247. Springer,Berlin – reference: Nichols DJ, Johnson KR (2008) Plants and the K-T boundary,Cambridge Univ. Press, United Kingdom – reference: Goldin TJ, Melosh HJ (2009) Self-shielding of thermalradiation by Chicxulub impact ejecta: Firestorm or fizzle?Geology, 37:1135-1138 – reference: Melosh HJ, Schneider NM, Zahnle KJ, Latham D (1990)Ignition of global wildfires at the Cretaceous/Tertiaryboundary. Nature, 343:251-254 – reference: Wilf P, Johnson KR, Huber BT (2003) Correlated terrestrialand marine evidence for global climate changes beforemass extinction at the Cretaceous-Paleogene boundary.Proceedings of National Academy of Science, 100:599-604 – reference: Hallam A, Perch-Nielsen K (1990) The biotic record ofevents in the marine realm at the end of the Cretaceous:calcareous, siliceous and organic-walled microfossils andmacroinvertebrates. Tectonophysics, 171:347-357 – reference: Zachos JC, Arthur MA, Dean W (1989) Geochemical evidencefor suppression of marine productivity at the Cretaceous/Tertiary boundary. Nature, 337:61-64 – reference: Adams JB, Mann ME, D’Hondt S (2004) The Cretaceous-Tertiary extinction: Modeling carbon flux and ecologicalresponse. Paleoceanography, 19:PA1002 – reference: Pope KO (2002) Impact dust not the cause of the Cretaceous-Tertiary mass extinction. Geology 30:99-102 – reference: Hollis CJ, Rodgers KA, Parker RJ (1995) Siliceous planktonbloom in the earliest Tertiary of Marlborough, New Zealand.Geology, 23:835-838 – reference: Pierazzo E, Hahmann AN, Sloan LC (2003) Chicxulub andclimate: radiative perturbations of impact-produced S-bearinggases. Astrobiology, 3:99-118 – reference: Kring DA, Durda DD (2002) Trajectories and distributionof material ejected from the Chicxulub impact crater:Implications for post impact wildfires. Journal of GeophysicalResearch, 107:6-22 – reference: Sheehan PM, Fastovsky DE (1992) Major extinctions of landdwellingvertebrates at the Cretaceous-Tertiary boundary,eastern Montana. Geology, 20:556-560 – reference: Vajda V, Raine JI, Hollis CJ (2001) Indication of globaldeforestation at the Cretaceous-Tertiary boundary by NewZealand fern spike. Science 294:1700-1702 – reference: 高橋 昭紀, 後藤, 和久 (2010) 恐竜絶滅研究の最前線. 科学,80:945-953 – reference: Belcher CM, Collinson ME, Sweet AR, Hildebrand AR, ScottAC (2003) Fireball Passes and Nothing Burns - The Roleof Thermal Radiation in the K-T Event: Evidence from theCharcoal Record of North America. Geology, 31:1061-1064 – reference: Harvey M, Brassell SC, Belcher CM, Montanari A, (2008)Combustion of fossil organic matter at the CretaceousPaleogene (K-P) boundary. Geology, 36:355-358 – reference: Miya M, Friedman M, Satoh TP, Takeshima H, Sado T, IwasakiW, Yamanoue Y, Nakatani M, Mabuchi K, Inoue JG, PoulsenJY, Fukunaga T, Sato Y, Nishida M (2013) EvolutionaryOrigin of the Scombridae (Tunas and Mackerels): Membersof a Paleogene Adaptive Radiation with 14 Other PelagicFish Families. PLOS ONE, 8:e73535. – reference: Pierazzo E, Kring DA, Melosh HJ (1998) Hydrocode simulationof the Chicxulub impact event and the production ofclimatically active gases. Journal of Geophysical Research,103:28607-28625. – reference: Sheehan PM, Hansen TA (1986) Detritus feeding as a buffer toextinction at the end of the Cretaceous. Geology, 14:868-870 – reference: Belcher CM (2009) Reigniting the Cretaceous-PalaeogeneFirestorm Debate. Geology, 37:1147-1148. – reference: Bown PR (2005) Selective calcareous nannoplanktonsurvivorship at the Cretaceous-Tertiary boundary. Geology,33:653-656 – reference: Sweet AR, Braman DR (2001) Cretaceous-Tertiary palynofloralperturbations and extinctions with the AquilapollenitesPhytogeographic Province. Canadian Journal of EarthSciences, 38:249-269 |
| SSID | ssib020382071 ssib044754498 ssib000195678 ssib012292016 ssib020472913 ssib002223873 ssib030454300 ssib000936954 ssib023160789 ssj0000564096 ssib031740835 |
| Score | 1.9961123 |
| Snippet | 白亜紀/古第三紀境界の大量絶滅は、地球史の中でも有数規模であった。絶滅は、特に光合成生物とそれを直接的な基盤とする生食連鎖に属する生物について顕著であるのに... |
| SourceID | affrit nii jstage |
| SourceType | Open Access Repository Publisher |
| StartPage | 39 |
| SubjectTerms | 光合成 大量絶滅 小惑星衝突 白亜紀/古第三紀境界 |
| Title | 大量絶滅の引き金になった食物連鎖の崩壊(<特集2>白亜紀末の大量絶滅事変に残る謎) |
| URI | https://www.jstage.jst.go.jp/article/seitai/64/1/64_KJ00009328568/_article/-char/ja https://cir.nii.ac.jp/crid/1390001204291966464 https://agriknowledge.affrc.go.jp/RN/2010872241 |
| Volume | 64 |
| hasFullText | 1 |
| inHoldings | 1 |
| isFullTextHit | |
| isPrint | |
| ispartofPNX | 日本生態学会誌, 2014/03/30, Vol.64(1), pp.39-46 |
| journalDatabaseRights | – providerCode: PRVAFT databaseName: Open Access Digital Library customDbUrl: eissn: 2424-127X dateEnd: 99991231 omitProxy: true ssIdentifier: ssib012292016 issn: 0021-5007 databaseCode: KQ8 dateStart: 20060101 isFulltext: true titleUrlDefault: http://grweb.coalliance.org/oadl/oadl.html providerName: Colorado Alliance of Research Libraries – providerCode: PRVHPJ databaseName: ROAD: Directory of Open Access Scholarly Resources customDbUrl: eissn: 2424-127X dateEnd: 99991231 omitProxy: true ssIdentifier: ssib044754498 issn: 0021-5007 databaseCode: M~E dateStart: 19540101 isFulltext: true titleUrlDefault: https://road.issn.org providerName: ISSN International Centre |
| link | http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwnV1PaxQxFB_aiuBF_ItVKz0YUGTrTCbJJCDCzHZKqeiphd6Gmd3Zsntoa2kPepCuoKUWKx4UxEIPLUit9FQFq36a7Xbdb-F7mZndWRSsXkI2eXlJ3pvZ_N6b5MUwrgtOyzyCh7fEI1VgTsQLyonNgpJlaUZxpLjejHn_gRifYhPTfLqvfyG3a2lpMRopPf7juZL_0SqUgV7xlOw_aLbDFAogD_qFFDQM6bF0THxOXEZch_iKgFUvx4jvEI8TTxBfEM8jkhPfBrRIXB-JvSJRWYkcTVspK6PxsoybZew0o8aQGH4q3YWEvNLNTU0DGZ8o0dsX0zQcCaQLQJbYxbStp9sqGJ6gxPaxVEEpDIgRzyVK00F74A7TgJ_dkfnHm7PmI72UGLrszlAgE5kwpDojiVvECaROkVomXOjaIS7PxqBHpZgWgcBeUv6jxBW6RxCuq7lB1x3nsxYFdFjEGuTHbmGRorqIoSyS24Qy34vV9briO-yXOstTtsMW8P0EYJzZ_IpDrQI3k5t9R2JdhidyChZ1pvOrUBLLvedtS5aUJNZTCk4Sd-1vy54EOxSf8Bj9SSOCjVhB1qwnljjGBzSVtEyJAR9OUAfQGW53feLnIT8XuRBvJt74yHvOTtuyC3ktiteddU0MatqAKbsmBsVopLkv4WBOiPwNB_ihntndEJEAZ5mZCwGI8SgZS10CSbx-wUx97V5HtGnELhTC7V4RAKwMK5WFKhqNNbC2MIxG_2y1moOQk2eM06ntN-wmL_JZo68WnjNOJgp-dN542Nz-0F551fr85ejbs0Z9r_n9TaP-sr3yulHfbdQ_Nupbjfpme2uztbrTXt5qr79Fmv2d5taLG3daq1_b75_Tu613Pw4PNlr7y0cbu1id43h4sNbcXgVeR3trjadrPz-t37xgTI35k8XxQnojSiGkwmEFBvaUoyJTxCGPKpUylaGUkYqZFcnQpiq2HKdSKpfMiDPJQhvRO48BSIQxoxEX9kVjYHZuNr5kDDt2JKJYAboPwYgo2yGtSK4cMDcYqwAOGDTMRHRBOLPQdfAHOhw9VJSCmbmgNh-YVoBf-0Gr1qBRTIQczCeRcoL0nzFItBIIFliY3JvQpqlNJReyQ4THTINaOGgMgYaCUhVTsE-1rxxhM2AFwQS7_Jf6K8YpfFUTN-lVY2BxYSkeAsNhMbqmn_Rf_Vfsfg |
| linkProvider | ISSN International Centre |
| openUrl | ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=%E5%A4%A7%E9%87%8F%E7%B5%B6%E6%BB%85%E3%81%AE%E5%BC%95%E3%81%8D%E9%87%91%E3%81%AB%E3%81%AA%E3%81%A3%E3%81%9F%E9%A3%9F%E7%89%A9%E9%80%A3%E9%8E%96%E3%81%AE%E5%B4%A9%E5%A3%8A%28%3C%E7%89%B9%E9%9B%862%3E%E7%99%BD%E4%BA%9C%E7%B4%80%E6%9C%AB%E3%81%AE%E5%A4%A7%E9%87%8F%E7%B5%B6%E6%BB%85%E4%BA%8B%E5%A4%89%E3%81%AB%E6%AE%8B%E3%82%8B%E8%AC%8E%29&rft.jtitle=%E6%97%A5%E6%9C%AC%E7%94%9F%E6%85%8B%E5%AD%A6%E4%BC%9A%E8%AA%8C&rft.au=%E5%BE%8C%E8%97%A4+%E5%92%8C%E4%B9%85&rft.date=2014&rft.pub=The+Ecological+Society+of+Japan&rft.issn=0021-5007&rft.eissn=2424-127X&rft.volume=64&rft.issue=1&rft.spage=39&rft.epage=46&rft_id=info:doi/10.18960%2Fseitai.64.1_39&rft.externalDocID=110009810891 |
| thumbnail_l | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=0021-5007&client=summon |
| thumbnail_m | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=0021-5007&client=summon |
| thumbnail_s | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=0021-5007&client=summon |