Continental configuration controls ocean oxygenation during the Phanerozoic.
Journal
Nature
ISSN: 1476-4687
Titre abrégé: Nature
Pays: England
ID NLM: 0410462
Informations de publication
Date de publication:
08 2022
08 2022
Historique:
received:
17
09
2021
accepted:
23
06
2022
entrez:
17
8
2022
pubmed:
18
8
2022
medline:
20
8
2022
Statut:
ppublish
Résumé
The early evolutionary and much of the extinction history of marine animals is thought to be driven by changes in dissolved oxygen concentrations ([O
Identifiants
pubmed: 35978129
doi: 10.1038/s41586-022-05018-z
pii: 10.1038/s41586-022-05018-z
doi:
Substances chimiques
Oxygen
S88TT14065
Types de publication
Historical Article
Journal Article
Langues
eng
Sous-ensembles de citation
IM
Pagination
523-527Commentaires et corrections
Type : CommentIn
Informations de copyright
© 2022. The Author(s), under exclusive licence to Springer Nature Limited.
Références
Payne, J. L. et al. Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity. Proc. Natl Acad. Sci. USA 106, 24–27 (2009).
pubmed: 19106296
doi: 10.1073/pnas.0806314106
Cole, D. B. et al. On the co-evolution of surface oxygen levels and animals. Geobiology 18, 260–281 (2020).
pubmed: 32175670
doi: 10.1111/gbi.12382
Sperling, E. A., Knoll, A. H. & Girguis, P. R. The ecological physiology of Earth’s second oxygen revolution. Annu. Rev. Ecol. Evol. Syst. 46, 215–235 (2015).
doi: 10.1146/annurev-ecolsys-110512-135808
Krause, A. J. et al. Stepwise oxygenation of the Paleozoic atmosphere. Nat. Commun. 9, 4081 (2018).
pubmed: 30287825
pmcid: 6172248
doi: 10.1038/s41467-018-06383-y
Tostevin, R. & Mills, B. J. Reconciling proxy records and models of Earth’s oxygenation during the Neoproterozoic and Palaeozoic. Interface Focus 10, 20190137 (2020).
pubmed: 32642053
pmcid: 7333907
doi: 10.1098/rsfs.2019.0137
Kocsis, Á. T., Reddin, C. J., Alroy, J. & Kiessling, W. The R package divDyn for quantifying diversity dynamics using fossil sampling data. Methods Ecol. Evol. 10, 735–743 (2019).
doi: 10.1111/2041-210X.13161
Penn, J. L., Deutsch, C., Payne, J. L. & Sperling, E. A. Temperature-dependent hypoxia explains biogeography and severity of end-Permian marine mass extinction. Science 362, eaat1327 (2018).
pubmed: 30523082
doi: 10.1126/science.aat1327
Edwards, C. T., Saltzman, M. R., Royer, D. L. & Fike, D. A. Oxygenation as a driver of the Great Ordovician Biodiversification Event. Nat. Geosci. 10, 925–929 (2017).
doi: 10.1038/s41561-017-0006-3
Dahl, T. W., Hammarlund, E. U. & Anbar, A. D. Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish. Proc. Natl Acad. Sci. 107, 17911–17915 (2010).
pubmed: 20884852
pmcid: 2964239
doi: 10.1073/pnas.1011287107
Zou, C. et al. Ocean euxinia and climate change “double whammy” drove the Late Ordovician mass extinction. Geology 46, 535–538 (2018).
doi: 10.1130/G40121.1
Bond, D., Wignall, P. B. & Racki, G. Extent and duration of marine anoxia during the Frasnian–Famennian (Late Devonian) mass extinction in Poland, Germany, Austria and France. Geol. Mag. 141, 173–193 (2004).
doi: 10.1017/S0016756804008866
Lau, K. V. et al. Marine anoxia and delayed Earth system recovery after the end-Permian extinction. Proc. Natl Acad. Sci. 113, 2360–2365 (2016).
pubmed: 26884155
pmcid: 4780601
doi: 10.1073/pnas.1515080113
Lu, W. et al. Late inception of a resiliently oxygenated upper ocean. Science 5, eaar5372 (2018).
doi: 10.1126/science.aar5372
Sperling, E. A. et al. A long-term record of early to mid-Paleozoic marine redox change. Sci. Adv. 7, eabf4382 (2021).
pubmed: 34233874
pmcid: 8262801
doi: 10.1126/sciadv.abf4382
Lenton, T. M. Earliest land plants created modern levels of atmospheric oxygen. Proc. Natl Acad. Sci. 113, 9704–9709 (2016).
pubmed: 27528678
pmcid: 5024600
doi: 10.1073/pnas.1604787113
Valdes, P., Scotese, C. & Lunt, D. Deep ocean temperatures through time. Clim. Past 17, 1483–1506 (2021).
doi: 10.5194/cp-17-1483-2021
Farnsworth, A. et al. Climate sensitivity on geological timescales controlled by nonlinear feedbacks and ocean circulation. Geophys. Res. Lett. 46, 9880–9889 (2019).
doi: 10.1029/2019GL083574
Scotese, C. R., Song, H., Mills, B. J. & van der Meer, D. G. Phanerozoic paleotemperatures: the earth’s changing climate during the last 540 million years. Earth Sci. Rev. 215, 103503 (2021).
doi: 10.1016/j.earscirev.2021.103503
Monteiro, F. M., Pancost, R. D., Ridgwell, A. & Donnadieu, Y. Nutrients as the dominant control on the spread of anoxia and euxinia across the Cenomanian-Turonian oceanic anoxic event (OAE2): model-data comparison. Paleoceanography 27, PA4209 (2012).
doi: 10.1029/2012PA002351
Ridgwell, A. et al. Marine geochemical data assimilation in an efficient Earth system model of global biogeochemical cycling. Biogeosciences 4, 87–104 (2007).
doi: 10.5194/bg-4-87-2007
Pohl, A. et al. Vertical decoupling in Late Ordovician anoxia due to reorganization of ocean circulation. Nat. Geosci. 14, 868–873 (2021).
doi: 10.1038/s41561-021-00843-9
Ward, B. A. et al. EcoGEnIE 1.0: plankton ecology in the cGENIE Earth system model. Geosci. Model Dev. 11, 4241–5267 (2018).
doi: 10.5194/gmd-11-4241-2018
Crichton, K. A., Wilson, J. D., Ridgwell, A. & Pearson, P. N. Calibration of temperature-dependent ocean microbial processes in the cGENIE.muffin (v0.9.13) Earth system model. Geosci. Model Dev. 14, 125–149 (2021).
doi: 10.5194/gmd-14-125-2021
Scotese, C. R. & Wright, N. PALEOMAP Paleodigital Elevation Models (PaleoDEMS) for the Phanerozoic. PALEOMAP Project. https://www.earthbyte.org/paleodem-resource-scotese-and-wright-2018/ (2018).
Pohl, A. et al. Quantifying the paleogeographic driver of Cretaceous carbonate platform development using paleoecological niche modeling. Palaeogeogr. Palaeoclimatol. Palaeoecol. 514, 222–232 (2019).
doi: 10.1016/j.palaeo.2018.10.017
Hülse, D. et al. End-Permian marine extinction due to temperature-driven nutrient recycling and euxinia. Nat. Geosci. 14, 862–867 (2021).
doi: 10.1038/s41561-021-00829-7
Baudin, F. & Riquier, L. The late Hauterivian Faraoni ‘oceanic anoxic event’: an update. Bull. Soc. Géol. Fr. 185, 359–377 (2014).
doi: 10.2113/gssgfbull.185.6.359
Laugié, M. et al. Exploring the impact of Cenomanian paleogeography and marine gateways on oceanic oxygen. Paleoceanogr. Paleoclimatol. 36, e2020PA004202 (2021).
doi: 10.1029/2020PA004202
De Vleeschouwer, D. et al. Timing and pacing of the Late Devonian mass extinction event regulated by eccentricity and obliquity. Nat. Commun. 8, 2268 (2017).
pubmed: 29273792
pmcid: 5741662
doi: 10.1038/s41467-017-02407-1
Ruvalcaba Baroni, I. et al. Ocean circulation in the Toarcian (Early Jurassic): a key control on deoxygenation and carbon burial on the European Shelf. Paleoceanogr. Paleoclimatol. 33, 994–1012 (2018).
doi: 10.1029/2018PA003394
Torsvik, T. H. BugPlates: Linking Biogeography and Palaeogeography (2009).
Ferreira, D., Marshall, J., Ito, T. & McGee, D. Linking glacial-interglacial states to multiple equilibria of climate. Geophys. Res. Lett. 45, 9160–9170 (2018).
doi: 10.1029/2018GL077019
Jaccard, S. L. & Galbraith, E. D. Large climate-driven changes of oceanic oxygen concentrations during the last deglaciation. Nat. Geosci. 5, 151–156 (2012).
doi: 10.1038/ngeo1352
Weijer, W. & Dijkstra, H. A. Multiple oscillatory modes of the global ocean circulation. J. Phys. Oceanogr. 33, 2197–2213 (2003).
doi: 10.1175/1520-0485(2003)033<2197:MOMOTG>2.0.CO;2
Sirkes, Z. & Tziperman, E. Identifying a damped oscillatory thermohaline mode in a general circulation model using an adjoint model. J. Phys. Oceanogr. 31, 2297–2306 (2001).
doi: 10.1175/1520-0485(2001)031<2297:IADOTM>2.0.CO;2
Meissner, K. J., Eby, M., Weaver, A. J. & Saenko, O. A. CO
doi: 10.1007/s00382-007-0279-0
Haarsma, R. J., Opsteegh, J. D., Selten, F. M. & Wang, X. Rapid transitions and ultra-low frequency behaviour in a 40 kyr integration with a coupled climate model of intermediate complexity. Clim. Dyn. 17, 559–570 (2001).
doi: 10.1007/s003820000129
Stolper, D. A. & Keller, C. B. A record of deep-ocean dissolved O
pubmed: 29310121
doi: 10.1038/nature25009
Brand, U. et al. Atmospheric oxygen of the Paleozoic. Earth Sci. Rev. 216, 103560 (2021).
doi: 10.1016/j.earscirev.2021.103560
Dahl, T. W. et al. Reorganisation of Earth’s biogeochemical cycles briefly oxygenated the oceans 520 Myr ago. Geochem. Perspect. Lett. 3, 210–220 (2019).
Wei, G. Y. et al. Global marine redox evolution from the late Neoproterozoic to the early Paleozoic constrained by the integration of Mo and U isotope records. Earth Sci. Rev. 214, 103506 (2021).
doi: 10.1016/j.earscirev.2021.103506
Wei, G. Y. et al. Marine redox fluctuation as a potential trigger for the Cambrian explosion. Geology 46, 587–590 (2018).
doi: 10.1130/G40150.1
Kendall, B. et al. Uranium and molybdenum isotope evidence for an episode of widespread ocean oxygenation during the late Ediacaran Period. Geochim. Cosmochim. Acta 156, 173–193 (2015).
doi: 10.1016/j.gca.2015.02.025
Dahl, T. W. et al. Brief oxygenation events in locally anoxic oceans during the Cambrian solves the animal breathing paradox. Sci Rep. 9, 11669 (2019).
pubmed: 31406148
pmcid: 6690889
doi: 10.1038/s41598-019-48123-2
Payne, J. L., Bachan, A., Heim, N. A., Hull, P. M. & Knope, M. L. The evolution of complex life and the stabilization of the Earth system. Interface Focus 10, 20190106 (2020).
pubmed: 32642051
pmcid: 7333899
doi: 10.1098/rsfs.2019.0106
Wilson, J. D., Monteiro, F. M., Schmidt, D. N., Ward, B. A. & Ridgwell, A. Linking marine plankton ecosystems and climate: a new modeling approach to the warm early Eocene climate. Paleoceanogr. Paleoclimatol. 33, 1439–1452 (2018).
doi: 10.1029/2018PA003374
Cao, L. et al. The role of ocean transport in the uptake of anthropogenic CO
doi: 10.5194/bg-6-375-2009
Reinhard, T. C. et al. Oceanic and atmospheric methane cycling in the cGENIE Earth system model – release v0.9.14. Geosci. Model Dev. 13, 5687–5706 (2020).
doi: 10.5194/gmd-13-5687-2020
van de Velde, S. J., Hülse, D., Reinhard, C. T. & Ridgwell, A. Iron and sulfur cycling in the cGENIE.muffin Earth system model (v0.9.21). Geosci. Model Dev. 14, 2713–2745 (2021).
doi: 10.5194/gmd-14-2713-2021
Müller, R. D., Sdrolias, M., Gaina, C., Steinberger, B. & Heine, C. Long-term sea-level fluctuations driven by ocean basin dynamics. Science 319, 1357–1362 (2008).
pubmed: 18323446
doi: 10.1126/science.1151540
Jacob, R. L. Low Frequency Variability in a Simulated Atmosphere-Ocean System.Thesis, Univ. Wisconsin (1997).
Crichton, K. A., Ridgwell, A., Lunt, D., Farnsworth, A. & Pearson, P. Data-constrained assessment of ocean circulation changes since the middle Miocene in an Earth system model. Clim. Past 17, 2223–2254 (2021).
doi: 10.5194/cp-17-2223-2021
Lê, S., Josse, J. & Husson, F. FactoMineR: an R package for multivariate analysis. J. Stat. Softw. 25, 1–18 (2008).
doi: 10.18637/jss.v025.i01
Weijer, W. et al. Stability of the Atlantic Meridional Overturning Circulation: a review and synthesis. J. Geophys. Res. Oceans 124, 5336–5375 (2019).
doi: 10.1029/2019JC015083
Ferreira, D., Marshall, J. & Campin, J. M. Localization of deep water formation: role of atmospheric moisture transport and geometrical constraints on ocean circulation. J. Clim. 23, 1456–1476 (2010).
doi: 10.1175/2009JCLI3197.1
Garcia, H. E. et al. World Ocean Atlas 2018, Volume 3: Dissolved Oxygen, Apparent Oxygen Utilization, and Dissolved Oxygen Saturation (National Oceanic and Atmospheric Administration, 2019).
Marsh, R. et al. Bistability of the thermohaline circulation identified through comprehensive 2-parameter sweeps of an efficient climate model. Clim. Dyn. 23, 761–777 (2004).
doi: 10.1007/s00382-004-0474-1
DeVries, T. & Holzer, M. Radiocarbon and helium isotope constraints on deep ocean ventilation and mantle-
doi: 10.1029/2018JC014716
Song, H. et al. The onset of widespread marine red beds and the evolution of ferruginous oceans. Nat. Commun. 8, 399 (2017).
pubmed: 28855507
pmcid: 5577183
doi: 10.1038/s41467-017-00502-x
Melchin, M. J., Mitchell, C. E., Holmden, C. & Štorch, P. Environmental changes in the Late Ordovician–early Silurian: review and new insights from black shales and nitrogen isotopes. Geol. Soc. Am. Bull. 125, 1635–1670 (2013).
doi: 10.1130/B30812.1
Pohl, A., Nardin, E., Vandenbroucke, T. R. A. & Donnadieu, Y. High dependence of Ordovician ocean surface circulation on atmospheric CO
doi: 10.1016/j.palaeo.2015.09.036
Meyer, K. M., Ridgwell, A. & Payne, J. L. The influence of the biological pump on ocean chemistry: implications for long-term trends in marine redox chemistry, the global carbon cycle, and marine animal ecosystems. Geobiology 14, 207–219 (2016).
pubmed: 26928862
pmcid: 5069655
doi: 10.1111/gbi.12176