H+ -driven increase in CO2 uptake and decrease in HCO3− uptake explain coccolithophores' acclimation responses to ocean acidification

اسناد مشابه

• The Influence of Sea Ice on Ocean Heat Uptake in Response to Increasing CO2

  مقاله‌ی دسترسی آزاد۲۰۰۶Journal of ClimateC. M.Bitz, P. R.Gent, R. A.Woodgate, M. M.Holland

• On the response of the oceanic wind-driven circulation to atmospheric CO2 increase

  سند علمی۲۰۰۵Oleg A. Saenko, John C. Fyfe, Matthew H. England

  A global, flux-corrected climate model is employed to predict the surface wind stress and associated wind-driven oceanic circulation for climate states corresponding to a doubling and quadrupling of the atmospheric CO2 concentration in a simple 1% per year CO2 increase scenario.

• Optimal uptake kinetics: physiological acclimation explains the pattern of nitrate uptake by phytoplankton in the ocean

  سند علمی۲۰۰۹S. Lan Smith, Yasuhiro Yamanaka, Markus Pahlow, Andreas Oschlies

  Phytoplankton supply the base of the marine food web and drive the biogeochemical cycles of carbon and nutrients. Over much of the ocean, their growth is limited by their uptake of nitrogen (as nitrate), which has most commonly been described by the hyperbolic Michaelis–Menten (M

• Optimal uptake kinetics: physiological acclimation explains the pattern of nitrate uptake by phytoplankton in the ocean

  مقاله‌ی دسترسی آزاد۲۰۰۹Marine Ecology Progress SeriesSLSmith, YYamanaka, MPahlow, AOschlies