Articles | Volume 15, issue 1
https://doi.org/10.5194/cp-15-105-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-15-105-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The 4.2 ka event, ENSO, and coral reef development
Lauren T. Toth
CORRESPONDING AUTHOR
US Geological Survey, St. Petersburg Coastal and Marine Science
Center, St. Petersburg, FL 33701, USA
Richard B. Aronson
Department of Ocean Engineering and Marine Sciences, Florida Institute
of Technology, Melbourne, FL 32901, USA
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Cited
24 citations as recorded by crossref.
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- New evidence for the periodic bleaching and recovery of Porites corals during the mid-late Holocene in the northern South China Sea H. Wang et al. 10.1016/j.gloplacha.2020.103397
- Spit-Inlet migration and storm-driven stacking at Praia de Leste Holocene barrier, southern Brazil M. Bogo et al. 10.1016/j.margeo.2021.106637
- Eemian (MIS 5e) climate oscillations based on palaeobotanical analysis from the Beckentin profile (NE Germany) A. Hrynowiecka et al. 10.1016/j.quaint.2021.01.025
- Surface oceanographic changes from ∼ 25,000 to 3500 cal yr BP in the eastern Arabian Sea J. Majumder et al. 10.1016/j.gloplacha.2024.104397
- ENSO may have contributed to sea level changes in the Gulf of Thailand during the Late-Holocene A. Jirapinyakul et al. 10.1177/09596836231197745
- Tropical Indian Ocean basin hydroclimate at the Mid- to Late-Holocene transition and the double drying hypothesis N. Scroxton et al. 10.1016/j.quascirev.2022.107837
- Hydroclimate variability in the Madagascar and Southeast African summer monsoons at the Mid- to Late-Holocene transition N. Scroxton et al. 10.1016/j.quascirev.2022.107874
- Holocene development and human use of mangroves and limestone forest at an ancient hong lagoon in the Tràng An karst, Ninh Binh, Vietnam S. O’Donnell et al. 10.1016/j.quascirev.2020.106416
- Vegetation and precipitation change inferred from the δ13C and δ2H values of n-alkanes from lake sediment from 18 cal ka BP, tropical NE Australia T. Li et al. 10.1016/j.quascirev.2024.108807
- The timing, duration and magnitude of the 8.2 ka event in global speleothem records S. Parker & S. Harrison 10.1038/s41598-022-14684-y
- How to Deal With Multi-Proxy Data for Paleoenvironmental Reconstructions: Applications to a Holocene Lake Sediment Record From the Tian Shan, Central Asia N. Schroeter et al. 10.3389/feart.2020.00353
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- Geochemical evidence of drying during the 4.2 ka event in sediment cores from the Yucatán Peninsula, Mexico D. Gibson et al. 10.1016/j.palaeo.2024.112527
- Upwelling buffers climate change impacts on coral reefs of the eastern tropical Pacific C. Randall et al. 10.1002/ecy.2918
- Climate changes in Northeastern Brazil from deglacial to Meghalayan periods and related environmental impacts G. Utida et al. 10.1016/j.quascirev.2020.106655
- Climate model experiments on the 4.2 ka event: The impact of tropical sea-surface temperature anomalies and desertification H. Renssen 10.1177/09596836221074031
- Sudden disappearance of yew (Taxus baccata) woodlands from eastern England coincides with a possible climate event around 4.2 ka ago T. Bebchuk et al. 10.1016/j.quascirev.2023.108414
- New definition for the subdivision of the Holocene Epoch and climate S. Hirabayashi & Y. Yokoyama 10.4116/jaqua.59.129
- Assigning causality to events in the Holocene record of coral reefs V. Rodriguez-Ruano et al. 10.1144/SP529-2022-47
- Inlet migration during the turning point between transgressive and regressive stages at the Guaratuba Holocene barrier, Paraná - Southern Brazil M. Bogo et al. 10.1016/j.margeo.2023.107048
- Spatial variability of sedimentary assemblages reflects variations in bioerosion pressure of adjacent coral reefs V. Rodriguez-Ruano et al. 10.1371/journal.pone.0311344
- Climate and the latitudinal limits of subtropical reef development L. Toth et al. 10.1038/s41598-021-87883-8
24 citations as recorded by crossref.
- Evidence from giant-clam <i>δ</i><sup>18</sup>O of intense El Ninõ–Southern Oscillation-related variability but reduced frequency 3700 years ago Y. Hu et al. 10.5194/cp-16-597-2020
- New evidence for the periodic bleaching and recovery of Porites corals during the mid-late Holocene in the northern South China Sea H. Wang et al. 10.1016/j.gloplacha.2020.103397
- Spit-Inlet migration and storm-driven stacking at Praia de Leste Holocene barrier, southern Brazil M. Bogo et al. 10.1016/j.margeo.2021.106637
- Eemian (MIS 5e) climate oscillations based on palaeobotanical analysis from the Beckentin profile (NE Germany) A. Hrynowiecka et al. 10.1016/j.quaint.2021.01.025
- Surface oceanographic changes from ∼ 25,000 to 3500 cal yr BP in the eastern Arabian Sea J. Majumder et al. 10.1016/j.gloplacha.2024.104397
- ENSO may have contributed to sea level changes in the Gulf of Thailand during the Late-Holocene A. Jirapinyakul et al. 10.1177/09596836231197745
- Tropical Indian Ocean basin hydroclimate at the Mid- to Late-Holocene transition and the double drying hypothesis N. Scroxton et al. 10.1016/j.quascirev.2022.107837
- Hydroclimate variability in the Madagascar and Southeast African summer monsoons at the Mid- to Late-Holocene transition N. Scroxton et al. 10.1016/j.quascirev.2022.107874
- Holocene development and human use of mangroves and limestone forest at an ancient hong lagoon in the Tràng An karst, Ninh Binh, Vietnam S. O’Donnell et al. 10.1016/j.quascirev.2020.106416
- Vegetation and precipitation change inferred from the δ13C and δ2H values of n-alkanes from lake sediment from 18 cal ka BP, tropical NE Australia T. Li et al. 10.1016/j.quascirev.2024.108807
- The timing, duration and magnitude of the 8.2 ka event in global speleothem records S. Parker & S. Harrison 10.1038/s41598-022-14684-y
- How to Deal With Multi-Proxy Data for Paleoenvironmental Reconstructions: Applications to a Holocene Lake Sediment Record From the Tian Shan, Central Asia N. Schroeter et al. 10.3389/feart.2020.00353
- 7700-year persistence of an isolated, free-living coral assemblage in the Galápagos Islands: a model for coral refugia? J. Feingold et al. 10.1007/s00338-020-01935-5
- Climatically driven Quaternary sedimentation in a passive margin tropical context: Insights into the geomorphological evolution of Northeastern Brazil D. Fonsêca et al. 10.1016/j.geomorph.2024.109316
- Geochemical evidence of drying during the 4.2 ka event in sediment cores from the Yucatán Peninsula, Mexico D. Gibson et al. 10.1016/j.palaeo.2024.112527
- Upwelling buffers climate change impacts on coral reefs of the eastern tropical Pacific C. Randall et al. 10.1002/ecy.2918
- Climate changes in Northeastern Brazil from deglacial to Meghalayan periods and related environmental impacts G. Utida et al. 10.1016/j.quascirev.2020.106655
- Climate model experiments on the 4.2 ka event: The impact of tropical sea-surface temperature anomalies and desertification H. Renssen 10.1177/09596836221074031
- Sudden disappearance of yew (Taxus baccata) woodlands from eastern England coincides with a possible climate event around 4.2 ka ago T. Bebchuk et al. 10.1016/j.quascirev.2023.108414
- New definition for the subdivision of the Holocene Epoch and climate S. Hirabayashi & Y. Yokoyama 10.4116/jaqua.59.129
- Assigning causality to events in the Holocene record of coral reefs V. Rodriguez-Ruano et al. 10.1144/SP529-2022-47
- Inlet migration during the turning point between transgressive and regressive stages at the Guaratuba Holocene barrier, Paraná - Southern Brazil M. Bogo et al. 10.1016/j.margeo.2023.107048
- Spatial variability of sedimentary assemblages reflects variations in bioerosion pressure of adjacent coral reefs V. Rodriguez-Ruano et al. 10.1371/journal.pone.0311344
- Climate and the latitudinal limits of subtropical reef development L. Toth et al. 10.1038/s41598-021-87883-8
Discussed (final revised paper)
Latest update: 11 Dec 2024
Short summary
We explore the hypothesis that a shift in global climate 4200 years ago (the 4.2 ka event) was related to the El Niño–Southern Oscillation (ENSO). We summarize records of coral reef development in the tropical eastern Pacific, where intensification of ENSO stalled reef growth for 2500 years starting around 4.2 ka. Because corals are highly sensitive to climatic changes, like ENSO, we suggest that records from coral reefs may provide important clues about the role of ENSO in the 4.2 ka event.
We explore the hypothesis that a shift in global climate 4200 years ago (the 4.2 ka event) was...
Special issue