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Response to Comment on "Sensitivity of seafloor bathymetry to climate-driven fluctuations in mid-ocean ridge magma supply"
Olive, J.-A.; Behn, M.D.; Ito, G.; Buck, W.R.; Escartin, J.; Howell, S. (2016). Response to Comment on "Sensitivity of seafloor bathymetry to climate-driven fluctuations in mid-ocean ridge magma supply". Science (Wash.) 353(6296): 229-c. http://dx.doi.org/10.1126/science.aaf2022
In: Science (Washington). American Association for the Advancement of Science: New York, N.Y. ISSN 0036-8075; e-ISSN 1095-9203, meer
Peer reviewed article  
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  • Olive, J.-A.
  • Behn, M.D.
  • Ito, G.
  • Buck, W.R.
  • Escartin, J.
  • Howell, S.
Abstract
    Tolstoy reports the existence of a characteristic 100 thousand year (ky) period in the bathymetry of fast-spreading seafloor but does not argue that sea level change is a first-order control on seafloor morphology worldwide. Upon evaluating the overlap between tectonic and Milankovitch periodicities across spreading rates, we reemphasize that fast-spreading ridges are the best potential recorders of a sea level signature in seafloor bathymetry.
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