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25th International Meeting on Organic Geochemistry IMOG 2011

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O-68<br />

Latitudinal distributi<strong>on</strong> of archaeal H-lipids<br />

Carme Huguet 1 , Susanne Fietz 1 , Ant<strong>on</strong>i Rosell-Melé 1,2<br />

1 aInstitut de Ciència i Tecnlogia Ambientals, Universitat Autònoma de Barcel<strong>on</strong>a, Cerdanyola, Spain,<br />

2 cInstitució Catalana de Recerca i Estudis Avançats (ICREA), Barcel<strong>on</strong>a, Spain (corresp<strong>on</strong>ding<br />

author:carme.huguet@uab.es)<br />

The unique compositi<strong>on</strong> of Archaea‘s membrane<br />

lipids allows them to maintain integrity and exchange<br />

capabilities in moderate and extreme c<strong>on</strong>diti<strong>on</strong>s 1 .<br />

They adapt to a wide range of temperatures by<br />

changing the number of rings in their glycerol dialkyl<br />

glycerol tetraether (GDGT) membrane lipids, which is<br />

used to estimate past water surface temperature via<br />

the TEX86 index 2 . Here we report that mesophile<br />

Archaea also synthesize an additi<strong>on</strong>al set of core<br />

membrane lipids with a covalent b<strong>on</strong>d between the<br />

two chains (H- GDGTs) which were previously<br />

thought to be restricted mainly to extremophiles 3 . We<br />

propose that these lipids help mesophile Archaea to<br />

adapt to cold c<strong>on</strong>diti<strong>on</strong>s, maintaining their membrane<br />

exchange capabilities. However, this c<strong>on</strong>tradicts<br />

previous hypothesis that suggested H-GDGTs to be<br />

an adaptati<strong>on</strong> to withstand high temperatures. We<br />

observe that H- GDGTs are widespread and<br />

abundant in mesophilic marine and lacustrine<br />

envir<strong>on</strong>ments, and that surprisingly they increase in<br />

abundance towards higher and colder latitudes (Fig.<br />

1). The lowest H-GDGT abundances (0-23%) were<br />

found between 0-45 ºN and 0-30 ºS str<strong>on</strong>gly<br />

increasing to 35-95% at 60-87ºN and 60-70ºS (Fig.<br />

a b<br />

1a). Moreover the c<strong>on</strong>tributi<strong>on</strong> of H-GDGTs increases<br />

as temperature decreases with values ranging from 0<br />

at 25 ºC to 95% below 0 ºC. In fact the relative H-<br />

GDGT abundance is significantly correlated with<br />

temperature (R²= 0.64 p

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