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Complete earth C (organic + inorganic) content ended up being significantly greater under local than exotic plantings, and differences increased with level. Remarkably, variations after eight years in C had been due to carbonate and never natural C fractions, where carbonate had been ~ 250 g C m-2 lower to at least one m earth depth under exotic than local plantings. Our results suggest that soil carbonate is an active share and that can react to variations in plant species traits over timescales of years. Sig
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