TROPICS cruise
GEOTRACES UK
GEOTRACES UK
with Gideon Henderson (Oxford University) and Alex Thomas (Edinburgh University)
NERC New Investigator Grant
Unravelling
the carbon cycle using silicon isotopes in the oceans
With
rising concerns surrounding the impacts of manmade climate change we
need to look not only into the future but also into the past. By
understanding how global temperatures and levels of carbon dioxide
(CO2) in the atmosphere have naturally fluctuated throughout the
earth's history, and the interaction with living organisms, we can
take important steps towards predicting the changes that may lie
ahead. It is undoubtedly a complex puzzle and there are many ways of
trying to solve it.
My
part of the story involves deep-sea sponges and silicon, the chemical
element they use to build their glass-like opal skeletons. Sponge
skeletons, or spicules, are helping me to piece together the links
between the supply of vital nutrients in different parts of the ocean
and the crucial role other marine organisms play in absorbing CO2
from the atmosphere and locking it away in deep sea sediments as
organic carbon.
Marine
sponges are one of the simplest groups of animals, living on the
seafloor and feeding by filtering particles from seawater. They
themselves don't play a central role in changing climates, but they
do share a common need for silicon with another group of marine
inhabitants that we think are vitally important to the global
climate. Diatoms, a type of microscopic marine algae that live and
photosynthesise at the sea surface, are responsible for sequestering
nearly half the CO2 that is converted into organic carbon and sinks
to the seafloor. By investigating sponges I can learn a lot about the
changing availability of silicon that also makes life possible for
diatoms.
A scanning electron microscope image of sponge spicules - K.Hendry, 2013 |
Studies
of ice-cores and ocean sediments tell us that over the past million
years the earth's climate has cycled every 100 thousand years or so
between cold ice ages, with low levels of atmospheric CO2, and warmer
periods, with higher CO2 levels. My studies focus on the climate
changes that took place since the end of the last ice age, around 15
thousand years ago. I can step back in time by combining analysis of
living sponges brought up from the deep during research cruises at
sea with fossil sponges taken from seafloor sediment samples.
I
was amongst the first to show that the chemical fingerprints of
sponges, in particular their silicon isotope composition, gives an
accurate record of how much silicon was dissolved in the water they
grew in. This opens up a unique archive stretching back millennia of
the silicon levels in ocean waters down to as much as 4 km beneath
the waves - the realm of sea sponges. In general, the more silicon
there is supplied to the sea surface, the more diatoms can grow, and
the more carbon dioxide they absorb and lock away in the seafloor
sediments when they die. Building a picture of past levels of silicon
in the oceans means I can test the crucial links between carbon
dioxide uptake by diatoms and climate change.
Here,
I plan to study key geographical areas, which have been sensitive to
rapid climate change since the last ice age.
My
work will provide essential insights into the dynamics of the carbon
cycle and hence climate, and point to possible future scenarios and
changes in ocean circulation patterns.
Leverhulme Research Project
Southern Ocean
Sponges: The link between biogeography and geochemistry
The Southern Ocean is a
key player in the regulation of global climate, through the upwelling
and formation of deep-water masses, the exchange of heat, carbon and
nutrients. Understanding the physical and chemical environment in
the Southern Ocean is essential for our understanding of
biogeographical distribution of marine organisms and the marine
carbon cycle. Our goal is to carry out a multidisciplinary study of
Southern Ocean sponges. We aim to provide taxomonic descriptions of
over 500 sponge specimens collected in the Southern Ocean; assess
biogeographical variation in assemblages, and the role of the
environment in sponge distribution; and carry out geochemical
analysis to assess further the silicon isotope variation between
different individuals and taxonomic groupings, to improve our
understanding of how sponges can be used as geochemical archives of
past ocean chemistry.
with Dr Claire Goodwin (National Museums Northern Ireland) and Dr Jade Berman (Ulster Wildlife Trust)
Marie Curie Career Integration Grant
Sailing in the Southern Ocean - photo K.Hendry, 2011 |
with Stephanie Bates and Kimberley Pyle (PhD students, Cardiff University)
Click here to find out about Kim and Steph's research trips.
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