Environmental records from coral skeletons
A decade of novel insights and innovation
Datos Bibliográficos
| ID | 12929136 |
|---|---|
| Autores | D M Thompson (0000-0002-6181-1259, University of Arizona, autor de correspondencia) |
| Año | 2021 |
| Volumen | 13 |
| Número | 1 |
| Fecha de publicación | 2021-10-26 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Wiley Interdisciplinary Reviews Climate Change (JOURNAL) |
| Identificadores de la revista | ISSN: 1757-7780 • E-ISSN: 1757-7799 |
| Editorial | Wiley (PUBLISHER • GB) |
| DOI | 10.1002/wcc.745 |
| OpenAlex | W3210866788 |
| Idioma | EN |
| Citas recibidas | 1 |
| Referencias citadas | 407 |
Hundreds of coral paleoclimate records have been developed over the past several decades, significantly extending the instrumental record and improving our understanding of tropical climate variability and change in otherwise data‐poor regions. Coral “proxy” records measure the change in skeletal geochemistry or growth as a function of ocean conditions at the time of calcification. Over the past decade (since 2010), new syntheses have identified coherent patterns of warming and variability that are unique within the paleo record (albeit not yet unprecedented). In turn, ocean warming and acidification have had a detrimental impact on coral growth, with reduced extension and increased stress banding. Methodological advances have constrained uncertainties and improved our understanding of the processes by which climate information is archived in coral skeletons. Models that describe these processes have been developed to facilitate proxy‐model comparisons, identify sources of uncertainties, and provide a benchmark upon which forced changes may be detected within a highly variable climate system. Finally, several innovative new proxies have expanded the climate and environmental information that may be obtained from corals, including: seawater pH, aragonite saturation, anthropogenic nitrogen, runoff, and trade winds. Further extending established and novel proxies should remain a priority, along with seawater monitoring and density measurements with which to screen and calibrate these records. As this critical climate archive is increasingly threatened by warming and ocean acidification, the community must work closely together to collect this invaluable climate data in an ecologically and culturally sensitive manner, before it is too late. This article is categorized under: Paleoclimates and Current Trends > Paleoclimate
Aragonite · Climate change · Climatology · Coral · Coral reef · Effects of global warming on oceans · Environmental change · Global warming · Ocean Acidification · Proxy (statistics · Coral and Marine Ecosystems Studies · Environmental Science · Ocean Acidification Effects and Responses · Oceanographic and Atmospheric Processes · Geology · Oceanography
U234U230Th232Th systematics and the precise measurement of time over the past 500,000 years
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Global warming and recurrent mass bleaching of corals
El Niño/Southern Oscillation and tropical Pacific climate during the last millennium
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The Community Earth System Model
Variability in the El Niño-Southern Oscillation Through a Glacial-Interglacial Cycle
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The Twentieth Century Reanalysis Project
Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization
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Extended Reconstructed Sea Surface Temperature, Version 5 (ERSSTv5)
Recent global-warming hiatus tied to equatorial Pacific surface cooling
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The ERA5 global reanalysis
Climate records from corals
Strong El Niño events during the early Holocene
Recent advances and future prospects of the U–Th and U–Pb chronometers applicable to archaeology
Simple, Rapid, and Cost Effective
Mass Spectrometric 14 C and U-Th Measurements in Coral
| Velocidad de citación | historical |
|---|---|
| Altamente citado | No |