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“The Quaternary Period, which began 2.6 million years ago (Ma), is subdivided into geochronological time units (epochs and ages), with boundaries linked at least in part to climate change events (expressed as Marine Isotope Stages), in association with paleomagnetic reversals ( 11 ).”
From The Anthropocene is functionally and stratigraphically distinct from the Holocene (2016) · cites this paper as [11]
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Crutzen, P. J. (2002) · Nature · doi:10.1038/415023a · Cited by 4,788
Intcal04 Terrestrial Radiocarbon Age Calibration, 0–26 Cal Kyr BP
(2004) · Radiocarbon · doi:10.1017/s0033822200032999 · Cited by 3,673
The Anthropogenic Greenhouse Era Began Thousands of Years Ago
Ruddiman, W. F. (2003) · Climatic Change · doi:10.1023/b:clim.0000004577.17928.fa · Cited by 1,658
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Self-citation
Metadata
- Authors
- Pillans, B., & Gibbard, P.
- ORCID
- Pillans, B.
- Venue
- The Geologic Time Scale
- Publisher
- Elsevier
- Published
- 2012
- Pages
- 979-1010
- OpenAlex
- W1960282296
- Cited by
- 157
- References
- 3
- Citations by year
- 2026: 2 · 2025: 6 · 2024: 10 · 2023: 5 · 2022: 7 · 2021: 15 · 2020: 6 · 2019: 24 · 2018: 13 · 2017: 14 · 2016: 15 · 2015: 11 · 2014: 12 · 2013: 10 · 2012: 3
- FWCI
- 23.91
- Type
- book chapter
- Language
- en
- Open access
- closed
- Locations
- Elsevier eBooks (publishedVersion)
- ANU Open Research (Australian National University) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- Quaternary, geologic time scale, stratigraphy, radiometric dating, stable isotopes, orbital tuning, stage boundaries, error analysis, Moon
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