Abstract
The formation of a global network of plate boundaries surrounding a mosaic of lithospheric fragments was a key step in the emergence of Earth’s plate tectonics. So far, propositions for plate boundary formation are regional in nature; how plate boundaries are created over thousands of kilometres in geologically short periods remains elusive. Here we show from geological observations that a >12,000-km-long plate boundary formed between the Indian and African plates around 105 Myr ago. This boundary comprised subduction segments from the eastern Mediterranean region to a newly established India–Africa rotation pole in the west Indian Ocean, where it transitioned into a ridge between India and Madagascar. We identify coeval mantle plume rise below Madagascar–India as the only viable trigger of this plate rotation. For this, we provide a proof of concept by torque balance modelling, which reveals that the Indian and African cratonic keels were important in determining plate rotation and subduction initiation in response to the spreading plume head. Our results show that plumes may provide a non-plate-tectonic mechanism for large-plate rotation, initiating divergent and convergent plate boundaries far away from the plume head. We suggest that this mechanism may be an underlying cause of the emergence of modern plate tectonics.
This is a preview of subscription content, access via your institution
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
$29.99 / 30 days
cancel any time
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
Data availability
GPlates files with reconstructions used to draft Fig. 1 are provided at https://figshare.com/articles/dataset/van_Hinsbergen_NatureGeo_2021_GPlates_zip/13516727.
Code availability
All codes used in the geodynamic modelling in this study are available at https://figshare.com/articles/software/van_Hinsbergen_etal_NatureGeo_2021_geodynamics_package/13635089.
References
Lenardic, A. The diversity of tectonic modes and thoughts about transitions between them. Phil. Trans. A 376, 20170416 (2018).
Stern, R. J. Subduction initiation: spontaneous and induced. Earth Planet. Sci. Lett. 226, 275–292 (2004).
Hall, C. E., Gurnis, M., Sdrolias, M., Lavier, L. L. & Müller, R. D. Catastrophic initiation of subduction following forced convergence across fracture zones. Earth Planet. Sci. Lett. 212, 15–30 (2003).
Gerya, T. V., Stern, R. J., Baes, M., Sobolev, S. V. & Whattam, S. A. Plate tectonics on the Earth triggered by plume-induced subduction initiation. Nature 527, 221–225 (2015).
Pusok, A. E. & Stegman, D. R. The convergence history of India–Eurasia records multiple subduction dynamics processes. Sci. Adv. 6, eaaz8681 (2020).
Baes, M., Sobolev, S., Gerya, T. & Brune, S. Plume-induced subduction initiation: single-slab or multi-slab subduction? Geochem. Geophys. Geosyst. 21, e2019GC008663 (2020).
Gurnis, M., Hall, C. & Lavier, L. Evolving force balance during incipient subduction. Geochem. Geophys. Geosyst. 5, Q07001 (2004)
Guilmette, C. et al. Forced subduction initiation recorded in the sole and crust of the Semail Ophiolite of Oman. Nat. Geosci. 11, 688–695 (2018).
Stern, R. J. & Gerya, T. Subduction initiation in nature and models: a review. Tectonophysics https://doi.org/10.1016/j.tecto.2017.10.014 (2017).
Agard, P. et al. Plate interface rheological switches during subduction infancy: control on slab penetration and metamorphic sole formation. Earth Planet. Sci. Lett. 451, 208–220 (2016).
van Hinsbergen, D. J. J. et al. Dynamics of intraoceanic subduction initiation: 2. Suprasubduction zone ophiolite formation and metamorphic sole exhumation in context of absolute plate motions. Geochem. Geophys. Geosyst. 16, 1771–1785 (2015).
Dilek, Y. & Furnes, H. Ophiolite genesis and global tectonics: geochemical and tectonic fingerprinting of ancient oceanic lithosphere. Geol. Soc. Am. Bull. 123, 387–411 (2011).
Gaina, C., van Hinsbergen, D. J. J. & Spakman, W. Tectonic interactions between India and Arabia since the Jurassic reconstructed from marine geophysics, ophiolite geology, and seismic tomography. Tectonics 34, 875–906 (2015).
Pourteau, A. et al. Thermal evolution of an ancient subduction interface revealed by Lu–Hf garnet geochronology, Halilbağı Complex (Anatolia). Geosci. Front. 10, 127–148 (2019).
Rioux, M. et al. Synchronous formation of the metamorphic sole and igneous crust of the Semail ophiolite: new constraints on the tectonic evolution during ophiolite formation from high-precision U–Pb zircon geochronology. Earth Planet. Sci. Lett. 451, 185–195 (2016).
Robinson, J., Beck, R., Gnos, E. & Vincent, R. K. New structural and stratigraphic insights for northwestern Pakistan from field and Landsat Thematic Mapper data. Geol. Soc. Am. Bull. 112, 364–374 (2000).
Parlak, O. The tauride ophiolites of Anatolia (Turkey): a review. J. Earth Sci. 27, 901–934 (2016).
van Hinsbergen, D. J. J. et al. Tectonic evolution and paleogeography of the Kırşehir Block and the Central Anatolian Ophiolites, Turkey. Tectonics 35, 983–1014 (2016).
Maffione, M., van Hinsbergen, D. J. J., de Gelder, G. I. N. O., van der Goes, F. C. & Morris, A. Kinematics of Late Cretaceous subduction initiation in the Neo-Tethys Ocean reconstructed from ophiolites of Turkey, Cyprus, and Syria. J. Geophys. Res. Solid Earth 122, 3953–3976 (2017).
van Hinsbergen, D. J., Maffione, M., Koornneef, L. M. & Guilmette, C. Kinematic and paleomagnetic restoration of the Semail ophiolite (Oman) reveals subduction initiation along an ancient Neotethyan fracture zone. Earth Planet. Sci. Lett. 518, 183–196 (2019).
Torsvik, T. H. & Cocks, L. R. M. Earth History and Palaeogeography (Cambridge Univ. Press, 2017).
Wan, B. et al. Cyclical one-way continental rupture-drift in the Tethyan evolution: subduction-driven plate tectonics. Sci. China Earth Sci. 62, 2005–2016 (2019).
van Hinsbergen, D. J. J. et al. Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic. Gondwana Res. 81, 79–229 (2020).
Warren, C. J., Parrish, R. R., Waters, D. J. & Searle, M. P. Dating the geologic history of Oman’s Semail ophiolite: insights from U–Pb geochronology. Contrib. Mineral. Petrol. 150, 403–422 (2005).
Güngör, T. et al. Kinematics and U–Pb zircon ages of the sole metamorphics of the Marmaris Ophiolite, Lycian Nappes, Southwest Turkey. Int. Geol. Rev. 61, 1124–1142 (2019).
van der Meer, D. G., van Hinsbergen, D. J. J. & Spakman, W. Atlas of the underworld: slab remnants in the mantle, their sinking history, and a new outlook on lower mantle viscosity. Tectonophysics 723, 309–448 (2018).
Buiter, S. J. & Torsvik, T. H. A review of Wilson Cycle plate margins: a role for mantle plumes in continental break-up along sutures? Gondwana Res. 26, 627–653 (2014).
Gibbons, A. D., Whittaker, J. M. & Müller, R. D. The breakup of East Gondwana: assimilating constraints from Cretaceous ocean basins around India into a best-fit tectonic model. J. Geophys. Res. Solid Earth 118, 808–822 (2013).
Gaina, C., Müller, R. D., Brown, B., Ishihara, T. & Ivanov, S. Breakup and early seafloor spreading between India and Antarctica. Geophys. J. Int. 170, 151–169 (2007).
Gaina, C. et al. The African Plate: a history of oceanic crust accretion and subduction since the Jurassic. Tectonophysics 604, 4–25 (2013).
Agard, P., Jolivet, L., Vrielynck, B., Burov, E. & Monié, P. Plate acceleration: the obduction trigger? Earth Planet. Sci. Lett. 258, 428–441 (2007).
Jolivet, L. et al. Neo-Tethys geodynamics and mantle convection: from extension to compression in Africa and a conceptual model for obduction. Can. J. Earth Sci. 53, 1190–1204 (2015).
Stampfli, G. M. & Borel, G. A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons. Earth Planet. Sci. Lett. 196, 17–33 (2002).
van Hinsbergen, D. J. J. et al. Reconstructing Greater India: paleogeographic, kinematic, and geodynamic perspectives. Tectonophysics 760, 69–94 (2019).
Kapp, P. & DeCelles, P. G. Mesozoic–Cenozoic geological evolution of the Himalayan–Tibetan orogen and working tectonic hypotheses. Am. J. Sci. 319, 159–254 (2019).
Advokaat, E. L. et al. Early Cretaceous origin of the Woyla Arc (Sumatra, Indonesia) on the Australian plate. Earth Planet. Sci. Lett. 498, 348–361 (2018).
Plunder, A. et al. History of subduction polarity reversal during arc‐continent collision: constraints from the Andaman Ophiolite and its metamorphic sole. Tectonics 39, e2019TC005762 (2020).
Torsvik, T. et al. Late Cretaceous magmatism in Madagascar: palaeomagnetic evidence for a stationary Marion hotspot. Earth Planet. Sci. Lett. 164, 221–232 (1998).
Mohan, M. R. et al. The Ezhimala igneous complex, southern India: possible imprint of late Cretaceous magmatism within rift setting associated with India–Madagascar separation. J. Asian Earth Sci. 121, 56–71 (2016).
Cande, S. C. & Stegman, D. R. Indian and African plate motions driven by the push force of the Reunion plume head. Nature 475, 47–52 (2011).
van Hinsbergen, D. J. J., Steinberger, B., Doubrovine, P. V. & Gassmöller, R. Acceleration and deceleration of India–Asia convergence since the Cretaceous: roles of mantle plumes and continental collision. J. Geophys. Res. https://doi.org/10.1029/2010jb008051 (2011).
Wang, Y. & Li, M. The interaction between mantle plumes and lithosphere and its surface expressions: 3-D numerical modelling. Geophys. J. Int. https://doi.org/10.1093/gji/ggab014 (2021).
Kumar, P. et al. The rapid drift of the Indian tectonic plate. Nature 449, 894–897 (2007).
Lamb, S. & Davis, P. Cenozoic climate change as a possible cause for the rise of the Andes. Nature 425, 792–797 (2003).
van der Meer, D. G., Spakman, W., van Hinsbergen, D. J. J., Amaru, M. L. & Torsvik, T. H. Towards absolute plate motions constrained by lower-mantle slab remnants. Nat. Geosci. 3, 36–40 (2010).
Tavani, S., Corradetti, A., Sabbatino, M., Seers, T. & Mazzoli, S. Geological record of the transition from induced to self-sustained subduction in the Oman Mountains. J. Geodyn. 133, 101674 (2020).
Tackley, P. J. Mantle convection and plate tectonics: toward an integrated physical and chemical theory. Science 288, 2002–2007 (2000).
Coltice, N., Husson, L., Faccenna, C. & Arnould, M. What drives tectonic plates? Sci. Adv. 5, eaax4295 (2019).
Dilek, Y. Ophiolite pulses, mantle plumes and orogeny. Geol. Soc. Lond. Spec. Publ. 218, 9–19 (2003).
Ernst, R., Grosfils, E. & Mege, D. Giant dike swarms: Earth, Venus, and Mars. Annu. Rev. Earth Planet. Sci. 29, 489–534 (2001).
Müller, R. D. et al. GPlates: building a virtual Earth through deep time. Geochem. Geophys. Geosyst. 19, 2243–2261 (2018).
Clube, T. M. M., Creer, K. M. & Robertson, A. H. F. Palaeorotation of the Troodos microplate, Cyprus. Nature 317, 522 (1985).
Morris, A., Meyer, M., Anderson, M. W. & MacLeod, C. J. Clockwise rotation of the entire Oman ophiolite occurred in a suprasubduction zone setting. Geology 44, 1055–1058 (2016).
McQuarrie, N. & van Hinsbergen, D. J. J. Retrodeforming the Arabia–Eurasia collision zone: age of collision versus magnitude of continental subduction. Geology 41, 315–318 (2013).
Monsef, I. et al. Evidence for an early-MORB to fore-arc evolution within the Zagros suture zone: constraints from zircon U–Pb geochronology and geochemistry of the Neyriz ophiolite (South Iran). Gondwana Res. 62, 287–305 (2018).
Galoyan, G. et al. Geology, geochemistry and 40Ar/39Ar dating of Sevan ophiolites (Lesser Caucasus, Armenia): evidence for Jurassic back-arc opening and hot spot event between the South Armenian Block and Eurasia. J. Asian Earth Sci. 34, 135–153 (2009).
Çelik, Ö. F. et al. Jurassic metabasic rocks in the Kızılırmak accretionary complex (Kargı region, Central Pontides, Northern Turkey). Tectonophysics 672–673, 34–49 (2016).
Topuz, G. et al. Jurassic ophiolite formation and emplacement as backstop to a subduction–accretion complex in northeast Turkey, the Refahiye ophiolite, and relation to the Balkan ophiolites. Am. J. Sci. 313, 1054–1087 (2014).
Ao, S. et al. U–Pb zircon ages, field geology and geochemistry of the Kermanshah ophiolite (Iran): from continental rifting at 79 Ma to oceanic core complex at ca. 36 Ma in the southern Neo-Tethys. Gondwana Res. 31, 305–318 (2016).
Peters, T. & Mercolli, I. Extremely thin oceanic crust in the Proto-Indian Ocean: evidence from the Masirah ophiolite, Sultanate of Oman. J. Geophys. Res. Solid Earth 103, 677–689 (1998).
Gnos, E. et al. Bela oceanic lithosphere assemblage and its relation to the Reunion hotspot. Terra Nova 10, 90–95 (1998).
Tapponnier, P., Mattauer, M., Proust, F. & Cassaigneau, C. Mesozoic ophiolites, sutures, and large-scale tectonic movements in Afghanistan. Earth Planet. Sci. Lett. 52, 355–371 (1981).
van Hinsbergen, D. J. J. et al. Greater India Basin hypothesis and a two-stage Cenozoic collision between India and Asia. Proc. Natl Acad. Sci. USA 109, 7659–7664 (2012).
Yuan, J. et al. Rapid drift of the Tethyan Himalaya terrane before two-stage India–Asia collision. Natl Sci. Rev. https://doi.org/10.1093/nsr/nwaa173 (2020).
Hébert, R. et al. The Indus–Yarlung Zangbo ophiolites from Nanga Parbat to Namche Barwa syntaxes, southern Tibet: first synthesis of petrology, geochemistry, and geochronology with incidences on geodynamic reconstructions of Neo-Tethys. Gondwana Res. 22, 377–397 (2012).
Zahirovic, S. et al. Tectonic evolution and deep mantle structure of the eastern Tethys since the latest Jurassic. Earth Sci. Rev. 162, 293–337 (2016).
Huang, W. et al. Lower Cretaceous Xigaze ophiolites formed in the Gangdese forearc: evidence from paleomagnetism, sediment provenance, and stratigraphy. Earth Planet. Sci. Lett. 415, 142–153 (2015).
Westerweel, J. et al. Burma Terrane part of the Trans-Tethyan arc during collision with India according to palaeomagnetic data. Nat. Geosci. 12, 863–868 (2019).
Jagoutz, O., Royden, L., Holt, A. F. & Becker, T. W. Anomalously fast convergence of India and Eurasia caused by double subduction. Nat. Geosci. 8, 475–478 (2015).
Höink, T. & Lenardic, A. Long wavelength convection, Poiseuille–Couette flow in the low-viscosity asthenosphere and the strength of plate margins. Geophys. J. Int. 180, 23–33 (2010).
Höink, T., Jellinek, A. M. & Lenardic, A. Viscous coupling at the lithosphere–asthenosphere boundary. Geochem. Geophys. Geosyst. 12, Q0AK02 (2011).
Campbell, I. H. Testing the plume theory. Chem. Geol. 241, 153–176 (2007).
Doubrovine, P. V., Steinberger, B. & Torsvik, T. H. A failure to reject: testing the correlation between large igneous provinces and deep mantle structures with EDF statistics. Geochem. Geophys. Geosyst. 17, 1130–1163 (2016).
Steinberger, B. Topography caused by mantle density variations: observation-based estimates and models derived from tomography and lithosphere thickness. Geophys. J. Int. 205, 604–621 (2016).
Steinberger, B. & Becker, T. W. A comparison of lithospheric thickness models. Tectonophysics 746, 325–338 (2018).
Acknowledgements
D.J.J.v.H. acknowledges funding through European Research Council Starting Grant 306810 (SINK) (also funding M.M., D.G., A.P. and E.L.A.), Netherlands Organization for Scientific Research (NWO) Vidi grant 864.11.004 (also funding K.P. and P.J.M.) and Netherlands Organization for Scientific Research (NWO) Vici grant 865.17.001. B.S. and C. Gaina received funding from the Research Council of Norway through its Centres of Excellence funding scheme, project no. 223272. B.S. acknowledges the innovation pool of the Helmholtz Association through the Advanced Earth System Modelling Capacity (ESM) activity. C. Guilmette was funded through Discovery Grant (RGPIN-2014-05681) from the National Science and Engineering Research Council of Canada. We thank I. L. ten Kate and D. Bandyopadhyay for discussion and F. Capitanio and D. Müller for their comments.
Author information
Authors and Affiliations
Contributions
D.J.J.v.H., B.S. and W.S. designed the research. D.J.J.v.H., C. Guilmette, M.M., D.G., K.P., A.P., P.J.M., C. Gaina, E.L.A. and R.L.M.V. developed the kinematic reconstruction; B.S. performed modelling; D.J.J.v.H., B.S., C. Guilmette and W.S. wrote the paper and all authors made corrections and edits.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Additional information
Peer review information Nature Geoscience thanks R. Dietmar Muller, Fabio Capitanio and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editor: Stefan Lachowycz.
Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Supplementary information
Supplementary Information
Supplementary Figs. 1–4.
Rights and permissions
About this article
Cite this article
van Hinsbergen, D.J.J., Steinberger, B., Guilmette, C. et al. A record of plume-induced plate rotation triggering subduction initiation. Nat. Geosci. 14, 626–630 (2021). https://doi.org/10.1038/s41561-021-00780-7
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41561-021-00780-7
This article is cited by
-
Horizontally forced initiation of the Izu-Bonin-Mariana subduction zone
Communications Earth & Environment (2024)
-
Intra-Oceanic Subduction Termination and Reinitiation of the Eastern Neo-Tethys in Myanmar
Journal of Earth Science (2024)
-
Formation of the Xigaze Metamorphic Sole under Tibetan continental lithosphere reveals generic characteristics of subduction initiation
Communications Earth & Environment (2023)
-
Paleogene India-Eurasia collision constrained by observed plate rotation
Nature Communications (2023)
-
The influence of Tethyan evolution on changes of the Earth’s past environment
Science China Earth Sciences (2023)