High-resolution analysis of the varved succession at Crawford lake across the base of the proposed Crawfordian stage and Anthropocene series
Dados Bibliográficos
| ID | 4189007 |
|---|---|
| Autores | Francine Mg Mccarthy (0000-0001-5038-8355, Brock University), Robert T Patterson (0000-0002-7760-2961, Carleton University), Carling R Walsh (0000-0002-1992-4532, Carleton University), Carling Walsh, Krysten M Lafond (0009-0003-2524-9427, Queen's University), Brian F Cummings (0000-0001-7254-3248, Queen's University), Andy B Cundy (0000-0003-4368-2569, University of Southampton), Karin Hain (0000-0001-5083-1986, University of Vienna), P Gaca (0000-0003-0786-3143, University of Southampton), Peter Steier (0000-0002-6144-2449, University of Vienna), Arnoud Boom (0000-0003-1299-691X, University of Leicester), Paul B Hamilton (0000-0001-6938-6341, Canadian Museum of Nature), Michael Fj Pisaric (0000-0003-3806-8986, Brock University), Martin J Head (0000-0003-3026-5483, Brock University), Joseph I Boyce (0000-0001-9083-6458, McMaster University), Nancy L Rose (0000-0002-5697-7334, University College London), D Turner (0000-0001-5603-8145), Simon D Turner (0000-0001-8692-8210, University College London) |
| Ano | 2025 |
| Volume | 12 |
| Fascículo | 2 |
| Páginas | 243-272 |
| Data de publicação | 2025-08-01 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | The Anthropocene Review (JOURNAL) |
| Identificadores do periódico | ISSN: 2053-0196 • E-ISSN: 2053-020X |
| Editora | SAGE Publications Inc (PUBLISHER) |
| DOI | 10.1177/20530196251315454 |
| PMID | 40756383 |
| OpenAlex | W4409443009 |
| Idioma | EN |
| Citações recebidas | 7 |
| Referências citadas | 39 |
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 239 + 240 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 239 + 240 Pu activities (calculated from atom concentrations of 239 Pu and 240 Pu measured using Accelerated Mass Spectrometry) of 0.0031 Bq/g between varves now assigned to 1951 and 1952 is consistent with the onset of thermonuclear weapons testing on November 1, 1952, so the proposed base for the Anthropocene is at the contact between the light- and dark-coloured laminae deposited in 1952 CE (17.5 cm in core CRA23-BC-1F-B). Sharply lower 239 + 240 Pu and 137 Cs activities capture the moratorium from November 1958 to September 1961 before rising quickly to peak activities of 239 + 240 Pu in 1963 CE. Analysis of individual varves with varying amounts of organic matter and inorganic calcite illustrates the influence of lithology on organic proxies, but the upcore trend toward depleted values of δ 15 N through the 20th C reflects increased fossil fuel combustion worldwide. An inflection point in δ 15 N around 1911 CE is attributed the global impact of the Haber-Bosch process and establishment of nearby steel mills, and another in the early 1950s attributed to the Great Acceleration to which the tipping point in the Earth system is attributed
Anthropocene · Chronology · Geochemistry · Geography · Global Boundary Stratotype Section and Point · Interglacial · Marine isotope stage · Physical geography · Quaternary · Radiometric dating · Sediment · Series (stratigraphy · Stage (stratigraphy · Stratotype · Varve · Isotope Analysis in Ecology · Radioactive contamination and transfer · Radioactivity and Radon Measurements · Geology · Paleontology
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Understanding the end of the Holocene
Chronostratigraphic grounds for the decision against formalizing an Anthropocene Epoch
Historical developments of Anthropocene concepts
Response to Damianos—Anthropocene angst
Before the Great Acceleration
A Possible Varving Mechanism for Meromictic Lakes
Fungal spores record Iroquoian and Canadian agriculture in 2nd millennium a.d. sediment of Crawford Lake, Ontario, Canada
Siliceous algae response to the “Great Acceleration” of the mid-20th century in Crawford Lake (Ontario, Canada)
The Anthropocene
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Humans and technology in the Anthropocene
Candidate sites and other reference sections for the Global boundary Stratotype Section and Point of the Anthropocene series
The Sihailongwan Maar Lake, northeastern China as a candidate Global boundary Stratotype Section and Point for the Anthropocene series
The Śnieżka peatland as a candidate Global boundary Stratotype Section and Point for the Anthropocene series
Evidence and experiment
Beppu Bay, Japan, as a candidate Global boundary Stratotype Section and Point for the Anthropocene series
The varved succession of Crawford Lake, Milton, Ontario, Canada as a candidate Global boundary Stratotype Section and Point for the Anthropocene series
The trajectory of the Anthropocene
| Obras citantes distintas | 7 |
|---|---|
| Citações por ano | 7 |
| Intervalo de citações | 2025 - 2026 (2) |
| Velocidade de citação | current |
| Altamente citado | Não |
| Tipos de citação | Neutras: 7 |