deLong, Kimberly; Blackburn, Terrence; Caissie, Beth; Addison, Jason A; Stroynowski, Zuzanna N; Reimi Sipala, Maria; Marcantonio, Franco; Ravelo, Ana Christina (2025): Silicon isotopes from IODP Site 323-U1340 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.974823
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Published: 2025-02-13 • DOI registered: 2025-03-14
Abstract:
The Bølling-Allerød deglacial event is marked by high diatom productivity and opal deposition throughout the subarctic Pacific. To investigate the cause of this event, we quantified several productivity-related sedimentary parameters that reflect the near-surface biogeochemistry from the Integrated Ocean Drilling Program (IODP) Site 323-U1340 in the Bering Sea. Silicon isotopes (δ29Si and δ30Si) from single-genus Coscinodiscus diatom frustules. Diatom silicon isotope values were generated in the Keck Laboratory at the University of California, Santa Cruz using the following methods. Freeze-dried samples were washed on a 63μm sieve to remove clays and dried in a 55°C oven. Samples were then cleaned with the M2 method, without the Calgon step, in non-glass containers and again oven-dried. To isolate a single diatom genus, samples were dry-sieved and ice rafted debris, radiolarians, spicules, and other genera were removed from the 63-125 μm portion by picking under a microscope and visually confirmed to be >99% Coscinodiscus specimens. Coscinodiscus species present were >95% Coscinodiscus marginatus with occasional Coscinodiscus oculus-iridis and Coscinodiscus radiatus. To dissolve samples, ≤0.002 g was transferred to 100 μL of 10 M NaOH in screw-top Teflon vials and reacted in Parr vessels at 200°C for three days. Samples were transferred to BioRad 50W X8 cation exchange columns previously cleaned with HCl and Milli-Q water (after Georg et al., 2006; doi:10.1016/j.chemgeo.2006.06.006), and eluted in Milli-Q water. Intensities of 28Si, 29Si and 30Si were measured using standard-sample bracketing on a Neptune MC ICP-MS at high resolution equipped with an Apex Omega desolvating nebulizer. All values are reported vs. NBS 28.
Keyword(s):
Supplement to:
deLong, Kimberly; Blackburn, Terrence; Caissie, Beth; Addison, Jason A; Stroynowski, Zuzanna N; Sipala, M R; Marcantonio, Franco; Ravelo, Ana Christina (2025): Bølling-Allerød Productivity in the Subarctic Pacific Driven by Seasonal Upwelling. Geophysical Research Letters, 52(8), e2024GL109614, https://doi.org/10.1029/2024GL109614
Coverage:
Median Latitude: 53.398896 * Median Longitude: -179.521415 * South-bound Latitude: 53.396673 * West-bound Longitude: -179.521623 * North-bound Latitude: 53.400013 * East-bound Longitude: -179.521000
Date/Time Start: 2009-07-22T00:00:00 * Date/Time End: 2009-07-22T00:00:00
Minimum Elevation: -1294.7 m * Maximum Elevation: -1293.4 m
Event(s):
323-U1340 * Latitude: 53.400000 * Longitude: -179.521000 * Date/Time: 2009-07-22T00:00:00 * Elevation: -1294.0 m * Location: Bering Sea * Campaign: Exp323 (Bering Sea Paleoceanography) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
323-U1340A * Latitude: 53.400013 * Longitude: -179.521622 * Elevation: -1294.7 m * Recovery: 535.91 m * Campaign: Exp323 (Bering Sea Paleoceanography) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 71 cores; 604.5 m cored; 89 % recovered
323-U1340D * Latitude: 53.396673 * Longitude: -179.521623 * Elevation: -1293.4 m * Recovery: 27.23 m * Campaign: Exp323 (Bering Sea Paleoceanography) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 3 cores; 26.3 m cored; 104 % recovered
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | deLong, Kimberly | |||
| 2 | Sample code/label | Sample label | deLong, Kimberly | DSDP/ODP/IODP sample designation | ||
| 3 | Half | Half | deLong, Kimberly | |||
| 4 | Depth, composite | Depth comp | mcd | deLong, Kimberly | IODP Depth Scale Terminology | |
| 5 | AGE | Age | ka BP | deLong, Kimberly | Age, 14C calibrated, CALIB (Stuiver & Reimer, 1993) | Geocode |
| 6 | δ29Si | δ29Si | ‰ NBS | deLong, Kimberly | Inductively coupled plasma mass spectrometer (ICP-MS), ThermoFisher Scientific, Neptune Plus; coupled with Apex Omega desolvating nebulizer | |
| 7 | δ29Si, standard deviation | δ29Si std dev | ± | deLong, Kimberly | Inductively coupled plasma mass spectrometer (ICP-MS), ThermoFisher Scientific, Neptune Plus; coupled with Apex Omega desolvating nebulizer | |
| 8 | δ30Si | δ30Si | ‰ NBS | deLong, Kimberly | Inductively coupled plasma mass spectrometer (ICP-MS), ThermoFisher Scientific, Neptune Plus; coupled with Apex Omega desolvating nebulizer | |
| 9 | δ30Si, standard deviation | δ30Si std dev | ± | deLong, Kimberly | Inductively coupled plasma mass spectrometer (ICP-MS), ThermoFisher Scientific, Neptune Plus; coupled with Apex Omega desolvating nebulizer | |
| 10 | Replicates | Repl | # | deLong, Kimberly |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
336 data points
Data
| 1 Event | 2 Sample label | 3 Half | 4 Depth comp [mcd] | 5 Age [ka BP] | 6 δ29Si [‰ NBS] | 7 δ29Si std dev [±] | 8 δ30Si [‰ NBS] | 9 δ30Si std dev [±] | 10 Repl [#] |
|---|---|---|---|---|---|---|---|---|---|
| 323-U1340A | 323-U1340A-1H-1,0-2 | Archive (A) | -0.050500 | 5.6919 | 0.68 | 0.04 | 1.35 | 0.0486 | 3 |
| 323-U1340A | 323-U1340A-1H-1,10-12 | Archive (A) | 0.049500 | 6.2123 | 0.64 | 0.12 | 1.27 | 0.0506 | 5 |
| 323-U1340A | 323-U1340A-1H-1,30-32 | Archive (A) | 0.249500 | 7.2530 | 0.73 | 0.05 | 1.44 | 0.0548 | 3 |
| 323-U1340A | 323-U1340A-1H-1,40-42 | Archive (A) | 0.349500 | 7.7734 | 0.66 | 0.19 | 1.44 | 0.0585 | 4 |
| 323-U1340A | 323-U1340A-1H-1,65-67 | Archive (A) | 0.599500 | 9.0742 | 0.68 | 0.02 | 1.43 | 0.0232 | 3 |
| 323-U1340A | 323-U1340A-1H-1,75-77 | Archive (A) | 0.699500 | 9.5946 | 0.79 | 0.00 | 1.55 | 0.0336 | 3 |
| 323-U1340A | 323-U1340A-1H-1,80-82 | Archive (A) | 0.749500 | 9.8548 | 0.78 | 0.05 | 1.58 | 0.0580 | 4 |
| 323-U1340A | 323-U1340A-1H-1,85-87 | Archive (A) | 0.799500 | 10.1150 | 0.78 | 0.02 | 1.54 | 0.0515 | 4 |
| 323-U1340A | 323-U1340A-1H-1,90-91 | Archive (A) | 0.844500 | 10.3491 | 0.87 | 0.06 | 1.70 | 0.0610 | 4 |
| 323-U1340A | 323-U1340A-1H-1,98-99 | Archive (A) | 0.924500 | 10.7654 | 0.77 | 0.04 | 1.50 | 0.0831 | 4 |
| 323-U1340A | 323-U1340A-1H-1,102-103 | Archive (A) | 0.964500 | 10.9735 | 0.73 | 0.06 | 1.63 | 0.0727 | 3 |
| 323-U1340A | 323-U1340A-1H-1,108-109 | Archive (A) | 1.024500 | 11.2858 | 0.80 | 0.05 | 1.51 | 0.0930 | 5 |
| 323-U1340A | 323-U1340A-1H-1,111-112 | Archive (A) | 1.054500 | 11.4419 | 0.71 | 0.13 | 1.53 | 0.0799 | 4 |
| 323-U1340A | 323-U1340A-1H-1,114-115 | Archive (A) | 1.084500 | 11.5980 | 0.76 | 0.01 | 1.52 | 0.0311 | 3 |
| 323-U1340A | 323-U1340A-1H-1,117-118 | Archive (A) | 1.114500 | 11.9300 | 0.70 | 0.04 | 1.41 | 0.0080 | 3 |
| 323-U1340A | 323-U1340A-1H-1,119-120 | Archive (A) | 1.134500 | 12.2170 | 0.79 | 0.17 | 1.47 | 0.0557 | 4 |
| 323-U1340A | 323-U1340A-1H-1,120-121 | Archive (A) | 1.144500 | 12.3500 | 0.80 | 0.04 | 1.60 | 0.0873 | 4 |
| 323-U1340A | 323-U1340A-1H-1,122-123 | Archive (A) | 1.164500 | 12.6300 | 0.83 | 0.03 | 1.61 | 0.0704 | 6 |
| 323-U1340A | 323-U1340A-1H-1,125-126 | Archive (A) | 1.194500 | 12.9259 | 0.80 | 0.04 | 1.54 | 0.0731 | 5 |
| 323-U1340A | 323-U1340A-1H-1,133-134 | Archive (A) | 1.274500 | 13.3843 | 0.81 | 0.02 | 1.53 | 0.0064 | 3 |
| 323-U1340A | 323-U1340A-1H-1,137-138 | Archive (A) | 1.314500 | 13.6135 | 0.71 | 0.01 | 1.39 | 0.0205 | 3 |
| 323-U1340A | 323-U1340A-1H-1,140-141 | Archive (A) | 1.344500 | 13.7854 | 0.85 | 0.03 | 1.60 | 0.0353 | 3 |
| 323-U1340A | 323-U1340A-1H-1,142-143 | Archive (A) | 1.364500 | 13.9000 | 0.82 | 0.01 | 1.57 | 0.0233 | 3 |
| 323-U1340A | 323-U1340A-1H-1,144-145 | Archive (A) | 1.384500 | 13.9230 | 0.81 | 0.09 | 1.46 | 0.0358 | 3 |
| 323-U1340A | 323-U1340A-1H-1,146-147 | Archive (A) | 1.404500 | 13.9544 | 0.82 | 0.11 | 1.62 | 0.0571 | 3 |
| 323-U1340A | 323-U1340A-1H-1,147-148 | Archive (A) | 1.414500 | 13.9701 | 0.76 | 0.02 | 1.49 | 0.0523 | 3 |
| 323-U1340A | 323-U1340A-1H-2,2-3 | Archive (A) | 1.464500 | 14.0485 | 0.86 | 0.09 | 1.52 | 0.0548 | 4 |
| 323-U1340A | 323-U1340A-1H-2,8-9 | Archive (A) | 1.524500 | 14.1427 | 0.77 | 0.05 | 1.52 | 0.0253 | 3 |
| 323-U1340A | 323-U1340A-1H-2,12-13 | Archive (A) | 1.564500 | 14.2054 | 0.81 | 0.05 | 1.54 | 0.0595 | 6 |
| 323-U1340A | 323-U1340A-1H-2,20-21 | Archive (A) | 1.644500 | 14.3309 | 0.81 | 0.05 | 1.58 | 0.0492 | 4 |
| 323-U1340A | 323-U1340A-1H-2,32-33 | Archive (A) | 1.764500 | 14.5192 | 0.90 | 0.01 | 1.68 | 0.0282 | 3 |
| 323-U1340A | 323-U1340A-1H-2,40-41 | Archive (A) | 1.844500 | 14.6457 | 0.75 | 0.00 | 1.64 | 0.0334 | 3 |
| 323-U1340A | 323-U1340A-1H-2,45-47 | Archive (A) | 1.899500 | 14.7501 | 0.80 | 0.02 | 1.52 | 0.0843 | 4 |
| 323-U1340A | 323-U1340A-1H-2,50-52 | Archive (A) | 1.949500 | 14.8450 | 0.70 | 0.04 | 1.40 | 0.0435 | 4 |
| 323-U1340A | 323-U1340A-1H-2,55-57 | Archive (A) | 1.999500 | 14.9399 | 0.72 | 0.05 | 1.44 | 0.1135 | 5 |
| 323-U1340A | 323-U1340A-1H-2,75-77 | Archive (A) | 2.199500 | 15.3196 | 0.71 | 0.01 | 1.47 | 0.0541 | 3 |
| 323-U1340A | 323-U1340A-1H-2,95-97 | Archive (A) | 2.399500 | 15.6992 | 0.75 | 0.11 | 1.53 | 0.1095 | 5 |
| 323-U1340A | 323-U1340A-1H-2,135-137 | Archive (A) | 2.799500 | 16.4586 | 0.64 | 0.19 | 1.36 | 0.0621 | 4 |
| 323-U1340A | 323-U1340A-1H-3,25-27 | Archive (A) | 3.199500 | 17.2179 | 0.98 | 0.03 | 1.86 | 0.0515 | 4 |
| 323-U1340D | 323-U1340D-1H-3,40-42 | Working (W) | 3.652243 | 18.0971 | 0.70 | 0.09 | 1.35 | 0.0710 | 4 |
| 323-U1340D | 323-U1340D-1H-3,86-88 | Working (W) | 4.132243 | 18.9413 | 0.82 | 0.02 | 1.61 | 0.0781 | 4 |
| 323-U1340D | 323-U1340D-1H-3,112-114 | Working (W) | 4.372243 | 19.4184 | 0.82 | 0.02 | 1.60 | 0.0732 | 4 |
