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author Huguet, Carme
de Lange, Gert J
Gustafsson, Örjan
Middelburg, Jack J
Sinninghe Damsté, Jaap S
Schouten, Stefan
author_facet Huguet, Carme
de Lange, Gert J
Gustafsson, Örjan
Middelburg, Jack J
Sinninghe Damsté, Jaap S
Schouten, Stefan
collection Datos científicos de ciencias marinas y ambientales
contents In ocean margin sediments both marine and terrestrial organic matter (OM) are buried but the factors governing their relative preservation and degradation are not well understood. In this study, we analysed the degree of preservation of marine isoprenoidal and soil-derived branched glycerol dialkyl glycerol tetraethers (GDGTs) upon long-term oxygen exposure in OM-rich turbidites from the Madeira Abyssal Plain by analyzing GDGT concentrations across oxidation fronts. Relative to the anoxic part of the turbidites ca. 7-20% of the soil-derived branched GDGTs were preserved in the oxidized part while only 0.2-3% of the marine isoprenoid GDGT crenarchaeol was preserved. Due to these different preservation factors the Branched Isoprenoid Tetraether (BIT) index, a ratio between crenarchaeol and the major branched GDGTs that is used as a tracer for soil-derived organic matter, substantially increases from 0.02 to 0.4. Split Flow Thin Cell (SPLITT) separation of turbidite sediments showed that the enhanced preservation of soil-derived carbon was a general phenomenon across the fine particle size ranges (<38 mm). Calculations reveal that, despite their relatively similar chemical structures, degradation rates of crenarchaeol are 2-fold higher than those of soil-derived branched GDGTs, suggesting preferential soil OM preservation possibly due to matrix protection.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_818287
institution PANGAEA
language en
publishDate 2008
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) TOC, δ¹³C, and preservation factors of turbidite sediments
Huguet, Carme
de Lange, Gert J
Gustafsson, Örjan
Middelburg, Jack J
Sinninghe Damsté, Jaap S
Schouten, Stefan
157-951; 157-952; Atlantic; Canarias Sea; Carbon, organic, total; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg157; North Atlantic Ocean; Ocean Drilling Program; ODP; PC; Piston corer; Preservation factor; Sample code/label; Tyro_90P22; δ13C, organic carbon
In ocean margin sediments both marine and terrestrial organic matter (OM) are buried but the factors governing their relative preservation and degradation are not well understood. In this study, we analysed the degree of preservation of marine isoprenoidal and soil-derived branched glycerol dialkyl glycerol tetraethers (GDGTs) upon long-term oxygen exposure in OM-rich turbidites from the Madeira Abyssal Plain by analyzing GDGT concentrations across oxidation fronts. Relative to the anoxic part of the turbidites ca. 7-20% of the soil-derived branched GDGTs were preserved in the oxidized part while only 0.2-3% of the marine isoprenoid GDGT crenarchaeol was preserved. Due to these different preservation factors the Branched Isoprenoid Tetraether (BIT) index, a ratio between crenarchaeol and the major branched GDGTs that is used as a tracer for soil-derived organic matter, substantially increases from 0.02 to 0.4. Split Flow Thin Cell (SPLITT) separation of turbidite sediments showed that the enhanced preservation of soil-derived carbon was a general phenomenon across the fine particle size ranges (<38 mm). Calculations reveal that, despite their relatively similar chemical structures, degradation rates of crenarchaeol are 2-fold higher than those of soil-derived branched GDGTs, suggesting preferential soil OM preservation possibly due to matrix protection.
title (Table 1) TOC, δ¹³C, and preservation factors of turbidite sediments
topic 157-951; 157-952; Atlantic; Canarias Sea; Carbon, organic, total; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg157; North Atlantic Ocean; Ocean Drilling Program; ODP; PC; Piston corer; Preservation factor; Sample code/label; Tyro_90P22; δ13C, organic carbon
url https://doi.org/10.1594/PANGAEA.818287