<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>12(2)</volume><submitter>McCarthy FM</submitter><funding>Natural Sciences and Engineering Research Council of Canada</funding><funding>Brock University</funding><funding>Haus der Kulturen der Welt</funding><funding>Kulturveranstaltungen des Bundes in Berlin</funding><pubmed_abstract>Four years after the Anthropocene Working Group (AWG) voted to work toward defining the Anthropocene series/epoch with a base in the mid-20th C, the varved sediments of Crawford Lake (Milton, ON, Canada) were selected as the Global boundary Stratotype Section and Point (GSSP) candidate. The initial major rise in activity of &lt;sup>239 + 240&lt;/sup>Pu had been selected as the primary chronostratigraphic marker to define the base of the Anthropocene, but the precise year when this occurred could not be determined from measurements of samples combining multiple varves. Individual varves from freeze cores collected in April 2023 provide annual resolution for bomb radionuclides, allowing the varve age model to be refined, former assignments determined to have been 1 year too old. The increase in &lt;s</pubmed_abstract><journal>The anthropocene review</journal><pagination>243-272</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12317751</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>High-resolution analysis of the varved succession at Crawford lake across the base of the proposed Crawfordian stage and Anthropocene series.</pubmed_title><pmcid>PMC12317751</pmcid><pubmed_authors>Head MJ</pubmed_authors><pubmed_authors>Cumming BF</pubmed_authors><pubmed_authors>Rose NL</pubmed_authors><pubmed_authors>Cundy AB</pubmed_authors><pubmed_authors>Gaca P</pubmed_authors><pubmed_authors>Steier P</pubmed_authors><pubmed_authors>Lafond KM</pubmed_authors><pubmed_authors>Hain K</pubmed_authors><pubmed_authors>Boyce JI</pubmed_authors><pubmed_authors>Patterson RT</pubmed_authors><pubmed_authors>Hamilton PB</pubmed_authors><pubmed_authors>Walsh C</pubmed_authors><pubmed_authors>Pisaric MF</pubmed_authors><pubmed_authors>McCarthy FM</pubmed_authors><pubmed_authors>Turner SD</pubmed_authors><pubmed_authors>Boom A</pubmed_authors></additional><is_claimable>false</is_claimable><name>High-resolution analysis of the varved succession at Crawford lake across the base of the proposed Crawfordian stage and Anthropocene series.</name><description>Four years after the Anthropocene Working Group (AWG) voted to work toward defining the Anthropocene series/epoch with a base in the mid-20th C, the varved sediments of Crawford Lake (Milton, ON, Canada) were selected as the Global boundary Stratotype Section and Point (GSSP) candidate. The initial major rise in activity of &lt;sup>239 + 240&lt;/sup>Pu had been selected as the primary chronostratigraphic marker to define the base of the Anthropocene, but the precise year when this occurred could not be determined from measurements of samples combining multiple varves. Individual varves from freeze cores collected in April 2023 provide annual resolution for bomb radionuclides, allowing the varve age model to be refined, former assignments determined to have been 1 year too old. The increase in &lt;s</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025 Aug</publication><modification>2026-03-15T22:18:53.679Z</modification><creation>2025-08-13T03:06:27.802Z</creation></dates><accession>S-EPMC12317751</accession><cross_references><pubmed>40756383</pubmed><doi>10.1177/20530196251315454</doi></cross_references></HashMap>