B. Fiałkiewicz-Kozieł, E. Łokas, Beata Smieja-Król, S. Turner, F. De Vleeschouwer, M. Woszczyk, K. Marcisz, M. Gałka, M. Lamentowicz, P. Kołaczek, I. Hajdas, Monika Karpińska-Kołaczek, Katarzyna Kołtonik, T. Mróz, S. Roberts, N. Rose, T. Krzykawski, A. Boom, Handong Yang
{"title":"作为人类世系列候选全球边界地层类型剖面和点的希尼卡泥炭地","authors":"B. Fiałkiewicz-Kozieł, E. Łokas, Beata Smieja-Król, S. Turner, F. De Vleeschouwer, M. Woszczyk, K. Marcisz, M. Gałka, M. Lamentowicz, P. Kołaczek, I. Hajdas, Monika Karpińska-Kołaczek, Katarzyna Kołtonik, T. Mróz, S. Roberts, N. Rose, T. Krzykawski, A. Boom, Handong Yang","doi":"10.1177/20530196221136425","DOIUrl":null,"url":null,"abstract":"The subalpine, atmospherically fed Śnieżka peatland, located in the Polish part of the Sudetes, is one of the nominated candidates for the GSSP of the Anthropocene. Data from two profiles, Sn1 (2012) and Sn0 (2020), from this site are critical for distinguishing the proposed epoch, while an additional core Sn2 is presented to support main evidence. The Sn0 archive contains a wide array of critical markers such as plutonium (Pu), radiocarbon (F14C), fly ash particles, Hg and stable C and N isotopes which are consistent with the previously well documented 210Pb/14C dated Sn1 profile, which provides a high-resolution and comprehensive database of trace elements and rare earth elements (REE), Pb isotopes, Pu, Cs, pollen and testate amoebae. The 1952 worldwide appearance of Pu, owing to its global synchronicity and repeatability between the cores, is proposed here as a primary marker of the Anthropocene, supported by the prominent upturn of selected chemostratigraphic and biostratigraphic indicators as well as the appearance of technofossils and artificial radionuclides.","PeriodicalId":74943,"journal":{"name":"The anthropocene review","volume":"10 1","pages":"288 - 315"},"PeriodicalIF":0.0000,"publicationDate":"2022-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"The Śnieżka peatland as a candidate Global boundary Stratotype Section and Point for the Anthropocene series\",\"authors\":\"B. Fiałkiewicz-Kozieł, E. Łokas, Beata Smieja-Król, S. Turner, F. De Vleeschouwer, M. Woszczyk, K. Marcisz, M. Gałka, M. Lamentowicz, P. Kołaczek, I. Hajdas, Monika Karpińska-Kołaczek, Katarzyna Kołtonik, T. Mróz, S. Roberts, N. Rose, T. Krzykawski, A. Boom, Handong Yang\",\"doi\":\"10.1177/20530196221136425\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The subalpine, atmospherically fed Śnieżka peatland, located in the Polish part of the Sudetes, is one of the nominated candidates for the GSSP of the Anthropocene. Data from two profiles, Sn1 (2012) and Sn0 (2020), from this site are critical for distinguishing the proposed epoch, while an additional core Sn2 is presented to support main evidence. The Sn0 archive contains a wide array of critical markers such as plutonium (Pu), radiocarbon (F14C), fly ash particles, Hg and stable C and N isotopes which are consistent with the previously well documented 210Pb/14C dated Sn1 profile, which provides a high-resolution and comprehensive database of trace elements and rare earth elements (REE), Pb isotopes, Pu, Cs, pollen and testate amoebae. The 1952 worldwide appearance of Pu, owing to its global synchronicity and repeatability between the cores, is proposed here as a primary marker of the Anthropocene, supported by the prominent upturn of selected chemostratigraphic and biostratigraphic indicators as well as the appearance of technofossils and artificial radionuclides.\",\"PeriodicalId\":74943,\"journal\":{\"name\":\"The anthropocene review\",\"volume\":\"10 1\",\"pages\":\"288 - 315\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-12-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"The anthropocene review\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1177/20530196221136425\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"The anthropocene review","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1177/20530196221136425","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The Śnieżka peatland as a candidate Global boundary Stratotype Section and Point for the Anthropocene series
The subalpine, atmospherically fed Śnieżka peatland, located in the Polish part of the Sudetes, is one of the nominated candidates for the GSSP of the Anthropocene. Data from two profiles, Sn1 (2012) and Sn0 (2020), from this site are critical for distinguishing the proposed epoch, while an additional core Sn2 is presented to support main evidence. The Sn0 archive contains a wide array of critical markers such as plutonium (Pu), radiocarbon (F14C), fly ash particles, Hg and stable C and N isotopes which are consistent with the previously well documented 210Pb/14C dated Sn1 profile, which provides a high-resolution and comprehensive database of trace elements and rare earth elements (REE), Pb isotopes, Pu, Cs, pollen and testate amoebae. The 1952 worldwide appearance of Pu, owing to its global synchronicity and repeatability between the cores, is proposed here as a primary marker of the Anthropocene, supported by the prominent upturn of selected chemostratigraphic and biostratigraphic indicators as well as the appearance of technofossils and artificial radionuclides.
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