Abstract
Fjords are connectors between the terrestrial and marine systems and are
known as globally significant hotspots for the burial (Smith et al.,
2014) and long-term storage (Smeaton et al., 2016) of carbon (C). The
glacial geomorphology of fjords and their catchment results in the
terrestrial and marine environments being strongly coupled more so than
other estuary types. The clearest example of this is the terrestrial C
subsidy to these sediment, it is estimated that globally 55-62% of C
held in fjord sediments are terrestrially derived (Cui et al., 2016).
Yet it is largely unknown how climatic and human forcing drives the
transfer of terrestrial C to the marine sediment. Here we, examine the
role of late Holocene climate and human activity on the transfer of C
from the terrestrial to marine environment along the North Atlantic
Margin. Loch Sunart a Scottish fjord sits at the land ocean interface of
the North Atlantic. The catchment of the fjord has been shown to be
sensitive to local and regional climatic change (Gillibrand et al.,
2005) and the fjord sediments have been able to record these changes in
Climate (Cage and Austin, 2010). Using a long (22m) sedimentary record
we will further develop our understanding of mid to late Holocene
regional climate and its impact on terrestrial C transfer to the coastal
ocean. Alongside this we will examine the role of humans on the
landscape and their impact on the transfer of terrestrial C on the
coastal ocean. The results from this study will further our
understanding of the long-term drivers of terrestrial C transfer to the
coastal ocean. Potentially this research provides insights on future C
transfers under a changing future climate allowing the importance of
fjords as a climate regulation service to be reassessed.
Original language | English |
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Pages | 7016 |
Publication status | Published - 1 Apr 2018 |