Stable Carbon Isotopes Suggest Large Terrestrial Carbon Inputs to the Global Ocean
|Author(s)||Kwon Eun Young1, 2, Devries Tim3, 4, Galbraith Eric D.5, 6, 7, 8, Hwang Jeomshik9, Kim Guebuem9, Timmermann Axel1, 2|
|Affiliation(s)||1 : Inst Basic Sci, Ctr Climate Phys, Busan, South Korea.
2 : Pusan Natl Univ, Busan, South Korea.
3 : Univ Calif Santa Barbara, Dept Geog, Santa Barbara, CA 93106, USA.
4 : Univ Calif Santa Barbara, Earth Res Inst, Santa Barbara, CA 93106 ,USA.
5 : ICREA, Pg Lluis Co 23, Barcelona, Spain.
6 : Univ Autonoma Barcelona, Inst Ciencia & Tecnol Ambientals ICTA, Barcelona, Spain.
7 : Univ Autonoma Barcelona, Dept Math, Barcelona, Spain.
8 : McGill Univ, Earth & Planetary Sci, Montreal, PQ, Canada.
9 : Seoul Natl Univ, Sch Earth & Environm Sci, Res Inst Oceanog, Seoul, South Korea.
|Source||Global Biogeochemical Cycles (0886-6236) (Amer Geophysical Union), 2021-04 , Vol. 35 , N. 4 , P. e2020GB006684 (25p.)|
|WOS© Times Cited||1|
The transport of carbon from land to ocean, via rivers, groundwater, and aerosols, is an important component of the global carbon cycle that must be known to accurately assess anthropogenic CO2 storage on land and in the ocean. Current global carbon cycle budgets have adopted terrestrial carbon inputs to the ocean ranging from 0.5 GtC/yr to 0.9 GtC/yr, derived mainly from estimates of riverine fluxes. However, these budgets ignore the terrestrial carbon inputs from coastal ecosystems and through submarine groundwater discharge (collectively referred to as coastal margin inputs in this study) due to difficulties in making global assessments. Using a numerical model and globally distributed ocean observations of stable carbon isotopes, we estimate terrestrial carbon inputs to the ocean at 1.4 +/- 0.5 GtC/yr, with 95% of the coastal margin inputs (0.8 +/- 0.5 GtC/yr) occurring in the Pacific and Indian Oceans. This terrestrial carbon flux is largely balanced by an efflux to the atmosphere of 1.2 +/- 0.5 GtC/yr, 40% of which occurs in poorly monitored coastal regions and may have been overlooked in previous observation-based global estimates. Our results suggest more dynamic cycling of carbon in the land-ocean transition zone than previously thought, and that rivers may not be the only important pathway for terrestrial carbon to the ocean.