Blue carbon storage capacity of temperate eelgrass (Zostera marina) meadows

MARIA EMILIA RÖHR; MARIANNE HOLMER; JULIA K. BAUM; MATS BJÖRK; KATHARYN E. BOYER; DIANA CHIN; LIA CHALIFOUR; STEPHANIE CIMON; MATHIEU CUSSON; MARTIN DAHL; DIANA DEYANOVA; J. EMMETT DUFFY; JOHAN S. EKLÖF; JULIE K. GEYER; JOHN N. GRIFFIN; MARTIN GULLSTRÖM; CLARA M. HEREU; MASAKAZU HORI; KEVIN A. HOVEL; A. RANDALL HUGHES; STEPHANIE L. KIRIAKOPOLOS; PABLO JORGENSEN; PER-OLAV MOKSNES; MASAHIRO NAKAOKA; MARY I. O'CONNOR; BRADLEY PETERSON; KATRIN REISS; PAMELA L. REYNOLDS; FRANCESCA ROSSI; JENNIFER L. RUESINK; RUI SANTOS,; JOHN J. STACHOWICZ; FIONA TOMAS; KUN-SEOP LEE; RICHARD K. F. UNSWORTH; CHRISTOFFER BOSTRÖM

GLOBAL BIOGEOCHEMICAL CYCLES

AMER GEOPHYSICAL UNION

Año: 2018 vol. 32 p. 1457 - 1475

0886-6236

Despite the importance of coastal ecosystems for the global carbon budgets, knowledge of their carbon storage capacity and the factors driving variability in storage capacity is still limited. Here we provide an estimate on the magnitude and variability of carbon stocks within a widely distributed marine foundation species throughout its distribution area in temperate Northern Hemisphere. We sampled 54 eelgrass (Zostera marina) meadows, spread across eight ocean margins and 36° of latitude, to determine abiotic and biotic factors influencing organic carbon (Corg) stocks in Zostera marina sediments. The Corg stocks (integrated over 25‐cm depth) showed a large variability and ranged from 318 to 26,523 g C/m2 with an average of 2,721 g C/m2. The projected Corg stocks obtained by extrapolating over the top 1 m of sediment ranged between 23.1 and 351.7 Mg C/ha, which is in line with estimates for other seagrasses and other blue carbon ecosystems. Most of the variation in Corg stocks was explained by five environmental variables (sediment mud content, dry density and degree of sorting, and salinity and water depth), while plant attributes such as biomass and shoot density were less important to Corg stocks. Carbon isotopic signatures indicated that at most sites <50% of the sediment carbon is derived from seagrass, which is lower than reported previously for seagrass meadows. The high spatial carbon storage variability urges caution in extrapolating carbon storage capacity between geographical areas as well as within and between seagrass species.