UK'37 and SST estimates of ODP Site 145-883

Here we present UK'37 and SST estimates from ODP site 883. Approximately 1–4 g of sediment was freeze-dried and homogenized prior to extraction with a Dionex 200 Accelerated Solvent Extractor using 100% dichloromethane. Prior to quantification, the total lipid extract was evaporated under N2 an...

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Hauptverfasser: Novak, Joseph B, Caballero-Gill, Rocio P, Rose, Rebecca, Herbert, Timothy D, Dowsett, Harry J
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Caballero-Gill, Rocio P
Rose, Rebecca
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Dowsett, Harry J
description Here we present UK'37 and SST estimates from ODP site 883. Approximately 1–4 g of sediment was freeze-dried and homogenized prior to extraction with a Dionex 200 Accelerated Solvent Extractor using 100% dichloromethane. Prior to quantification, the total lipid extract was evaporated under N2 and redissolved in 200 μL toluene spiked with n-hexatriacontane (C36) and n-heptatriacontane (C37) standards. Alkenone concentrations were calculated by comparison of C37:2 and C37:3 alkenone peak areas to the peak areas of the C36 and C37 internal standards determined by an Agilent Technologies 6890 gas chromatograph flame ionization detector (GC-FID), with an Agilent Technologies DB-1 column (60 m, 0.32 mm diameter, 0.10 mm film thickness). 1 μL of total lipid extract was injected at an initial temperature of 90°C, increasing to 255°C at 40°C/min, then to 300°C at 1°C/min, ramping to 320°C at 10°C/min, and ending with an isothermal hold at 320°C for 11 minutes. 228 of 504 samples from ODP 883 were analyzed at least in duplicate, yielding a mean analytical error equivalent to ±0.11°C.
doi_str_mv 10.1594/pangaea.967371
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Approximately 1–4 g of sediment was freeze-dried and homogenized prior to extraction with a Dionex 200 Accelerated Solvent Extractor using 100% dichloromethane. Prior to quantification, the total lipid extract was evaporated under N2 and redissolved in 200 μL toluene spiked with n-hexatriacontane (C36) and n-heptatriacontane (C37) standards. Alkenone concentrations were calculated by comparison of C37:2 and C37:3 alkenone peak areas to the peak areas of the C36 and C37 internal standards determined by an Agilent Technologies 6890 gas chromatograph flame ionization detector (GC-FID), with an Agilent Technologies DB-1 column (60 m, 0.32 mm diameter, 0.10 mm film thickness). 1 μL of total lipid extract was injected at an initial temperature of 90°C, increasing to 255°C at 40°C/min, then to 300°C at 1°C/min, ramping to 320°C at 10°C/min, and ending with an isothermal hold at 320°C for 11 minutes. 228 of 504 samples from ODP 883 were analyzed at least in duplicate, yielding a mean analytical error equivalent to ±0.11°C.</abstract><pub>PANGAEA</pub><doi>10.1594/pangaea.967371</doi><orcidid>https://orcid.org/0000-0002-8569-2645</orcidid><orcidid>https://orcid.org/0000-0003-1556-4290</orcidid><orcidid>https://orcid.org/0000-0003-1983-7524</orcidid><oa>free_for_read</oa></addata></record>
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identifier DOI: 10.1594/pangaea.967371
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recordid cdi_datacite_primary_10_1594_pangaea_967371
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subjects AGE
Age model
Alkenone, unsaturation index UK'37
Alkenone, unsaturation index UK'37, standard deviation
Alkenones
Benthic foraminifera assemblages
Benthic foraminiferal stable isotopes
Calcium Carbonate content
Calculated from UK'37 (Müller et al, 1998)
Composite splice
Depth, composite
DEPTH, sediment/rock
diatoms
Drilling/drill rig
DSDP/ODP/IODP sample designation
Event label
Joides Resolution
Leg145
Ocean Drilling Program (ODP)
ODP 883
ODP 887
Sample code/label
Sea surface temperature
Sea surface temperature, standard deviation
SST, from UK'37, BAYSPLINE (Tierney and Tingley, 2018)
stable carbon isotopes δ13C
stable oxygen isotopes
Subarctic North Pacific
Uk'37 sst and C37total
title UK'37 and SST estimates of ODP Site 145-883
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