Conventional analyses using this method estimate that Earth’s biosphere weighs about 560 billion tonnes C, with an annual productivity of 104.9 billion tonnes C/yr almost evenly split between terrestrial and marine environments, despite the oceans containing only 1.34% of all complex biomass. This total biomass is approximately 1/100,000,000 of the Earth’s solid mass (M⊕ = 5.97219 × 1021 tonnes) and 1/10,000 of the atmospheric mass (MA = 5.97 × 1015 tonnes) (Field et al., 1998; Groombridge & Jenkins, 2002; Gielen et al., 2003; Moreira, 2006; Djomo et al., 2010; Erb et al., 2009). Plant biomass, called lignocellulosic phytomass in fuel energy studies, contributes to these figures more than animal biomass. Based on chlorophyll levels from the normalized difference vegetation index (NDVI), the most biologically productive regions with autotrophic plants are
Conventional analyses using this method estimate that Earth’s biosphere weighs about 560 billion tonnes C, with an annual productivity of 104.9 billion tonnes C/yr almost evenly split between terrestrial and marine environments, despite the oceans containing only 1.34% of all complex biomass. This total biomass is approximately 1/100,000,000 of the Earth’s solid mass (M⊕ = 5.97219 × 1021 tonnes) and 1/10,000 of the atmospheric mass (MA = 5.97 × 1015 tonnes) (Field et al., 1998; Groombridge & Jenkins, 2002; Gielen et al., 2003; Moreira, 2006; Djomo et al., 2010; Erb et al., 2009). Plant biomass, called lignocellulosic phytomass in fuel energy studies, contributes to these figures more than animal biomass. Based on chlorophyll levels from the normalized difference vegetation index (NDVI), the most biologically productive regions with autotrophic plants are