High stocks, but slow recovery, of ecosystem carbon in southern oceanic tussock grasslands

• Published in: Polar Biology
• Main Authors: Smith, Stuart, Karlsson, Susanna
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Verlag 2017
• Subjects: Antarctic; Antarc*; Polar Biology
• Online Access: http://hdl.handle.net/11250/2596770; https://doi.org/10.1007/s00300-017-2084-5

Peat-forming large tussock grasslands on oceanic and sub-Antarctic islands are fundamentally understudied in terms of carbon (C) storage. Here we quantify both plant and soil C and nitrogen (N) storage for the large-tussock grass Poa flabellata in the Falkland Islands, at its most northerly range. In this study we adopt a spatially explicit sampling approach to accounting for tussock and inter-tussock (between tussocks) areas for three habitats; remnant stands (surviving clearance and overgrazing), restored stands (planted) and eroded bare peat sites. We found that remnant stands of P. flabellata have above-ground C densities of 49.8 ± 9.7 Mg C ha-1, equivalent to temperate and boreal forests. The majority of above-ground C is stored within the pedestal, a compact accumulation of dead leaves, rhizomes and roots. By surveying restored stands of increasing age we found that such C accrual may take longer than two decades. Soil C stocks were horizontally and vertically spatially variable and did not differ between habitat types. Plant and soil C and N stocks were strongly coupled identifying the important role of N availability for C accrual in this system. Scaling-up our results, planting tussock grass could accrue up to 0.9 million Mg C on a decadal timescale across the islands, yet the impact of planting on soil C storage is likely to be more variable. Our results highlight the local and regional importance of large tussock grasslands as dense C stores and that land management and conservation of these communities needs to be more carbon-conscious. acceptedVersion This is a post-peer-review, pre-copyedit version of an article published in [Polar Biology]. The final authenticated version is available online at: https://doi.org/10.1007/s00300-017-2084-5