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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creator | Novak, Joseph B Caballero-Gill, Rocio P Rose, Rebecca Herbert, Timothy D 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 |
format | Dataset |
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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.</description><identifier>DOI: 10.1594/pangaea.967371</identifier><language>eng</language><publisher>PANGAEA</publisher><subject>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</subject><creationdate>2024</creationdate><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0002-8569-2645 ; 0000-0003-1556-4290 ; 0000-0003-1983-7524</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>776,1888</link.rule.ids><linktorsrc>$$Uhttps://commons.datacite.org/doi.org/10.1594/pangaea.967371$$EView_record_in_DataCite.org$$FView_record_in_$$GDataCite.org$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Novak, Joseph B</creatorcontrib><creatorcontrib>Caballero-Gill, Rocio P</creatorcontrib><creatorcontrib>Rose, Rebecca</creatorcontrib><creatorcontrib>Herbert, Timothy D</creatorcontrib><creatorcontrib>Dowsett, Harry J</creatorcontrib><title>UK'37 and SST estimates of ODP Site 145-883</title><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.</description><subject>AGE</subject><subject>Age model</subject><subject>Alkenone, unsaturation index UK'37</subject><subject>Alkenone, unsaturation index UK'37, standard deviation</subject><subject>Alkenones</subject><subject>Benthic foraminifera assemblages</subject><subject>Benthic foraminiferal stable isotopes</subject><subject>Calcium Carbonate content</subject><subject>Calculated from UK'37 (Müller et al, 1998)</subject><subject>Composite splice</subject><subject>Depth, composite</subject><subject>DEPTH, sediment/rock</subject><subject>diatoms</subject><subject>Drilling/drill rig</subject><subject>DSDP/ODP/IODP sample designation</subject><subject>Event label</subject><subject>Joides Resolution</subject><subject>Leg145</subject><subject>Ocean Drilling Program (ODP)</subject><subject>ODP 883</subject><subject>ODP 887</subject><subject>Sample code/label</subject><subject>Sea surface temperature</subject><subject>Sea surface temperature, standard deviation</subject><subject>SST, from UK'37, BAYSPLINE (Tierney and Tingley, 2018)</subject><subject>stable carbon isotopes δ13C</subject><subject>stable oxygen isotopes</subject><subject>Subarctic North Pacific</subject><subject>Uk'37 sst and C37total</subject><fulltext>true</fulltext><rsrctype>dataset</rsrctype><creationdate>2024</creationdate><recordtype>dataset</recordtype><sourceid>PQ8</sourceid><recordid>eNpjYBAzNNAzNLU00S9IzEtPTE3UszQzNzY35GTQDvVWNzZXSMxLUQgODlFILS7JzE0sSS1WyE9T8HcJUAjOLElVMDQx1bWwMOZhYE1LzClO5YXS3Ax6bq4hzh66KYkliclAhfEFRUDdRZXxhgbxINviobbFQ2wzJlkDAJFQNds</recordid><startdate>2024</startdate><enddate>2024</enddate><creator>Novak, Joseph B</creator><creator>Caballero-Gill, Rocio P</creator><creator>Rose, Rebecca</creator><creator>Herbert, Timothy D</creator><creator>Dowsett, Harry J</creator><general>PANGAEA</general><scope>DYCCY</scope><scope>PQ8</scope><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></search><sort><creationdate>2024</creationdate><title>UK'37 and SST estimates of ODP Site 145-883</title><author>Novak, Joseph B ; Caballero-Gill, Rocio P ; Rose, Rebecca ; Herbert, Timothy D ; Dowsett, Harry J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-datacite_primary_10_1594_pangaea_9673713</frbrgroupid><rsrctype>datasets</rsrctype><prefilter>datasets</prefilter><language>eng</language><creationdate>2024</creationdate><topic>AGE</topic><topic>Age model</topic><topic>Alkenone, unsaturation index UK'37</topic><topic>Alkenone, unsaturation index UK'37, standard deviation</topic><topic>Alkenones</topic><topic>Benthic foraminifera assemblages</topic><topic>Benthic foraminiferal stable isotopes</topic><topic>Calcium Carbonate content</topic><topic>Calculated from UK'37 (Müller et al, 1998)</topic><topic>Composite splice</topic><topic>Depth, composite</topic><topic>DEPTH, sediment/rock</topic><topic>diatoms</topic><topic>Drilling/drill rig</topic><topic>DSDP/ODP/IODP sample designation</topic><topic>Event label</topic><topic>Joides Resolution</topic><topic>Leg145</topic><topic>Ocean Drilling Program (ODP)</topic><topic>ODP 883</topic><topic>ODP 887</topic><topic>Sample code/label</topic><topic>Sea surface temperature</topic><topic>Sea surface temperature, standard deviation</topic><topic>SST, from UK'37, BAYSPLINE (Tierney and Tingley, 2018)</topic><topic>stable carbon isotopes δ13C</topic><topic>stable oxygen isotopes</topic><topic>Subarctic North Pacific</topic><topic>Uk'37 sst and C37total</topic><toplevel>online_resources</toplevel><creatorcontrib>Novak, Joseph B</creatorcontrib><creatorcontrib>Caballero-Gill, Rocio P</creatorcontrib><creatorcontrib>Rose, Rebecca</creatorcontrib><creatorcontrib>Herbert, Timothy D</creatorcontrib><creatorcontrib>Dowsett, Harry J</creatorcontrib><collection>DataCite (Open Access)</collection><collection>DataCite</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Novak, Joseph B</au><au>Caballero-Gill, Rocio P</au><au>Rose, Rebecca</au><au>Herbert, Timothy D</au><au>Dowsett, Harry J</au><format>book</format><genre>unknown</genre><ristype>DATA</ristype><title>UK'37 and SST estimates of ODP Site 145-883</title><date>2024</date><risdate>2024</risdate><abstract>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.</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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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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