Smear slide grain counts from IODP Site 323-U1342

Here we present new grain count data from from Integrated Ocean Drilling Program (IODP) Expedition 323 Site U1342 Holes A, C, and D. New records of sediment composition from laminated and non-laminated were determined from smear slide (quantitative grain counts) and particle size analyses. A subset...

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Main Authors: Aiello, Ivano W, Knudson, Karla P, Ravelo, Ana Christina, Drake, Michelle K
Format: Dataset
Language:English
Published: PANGAEA
Subjects:
AGE
Run
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.933699
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.933699
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.933699 2024-09-15T17:59:36+00:00 Smear slide grain counts from IODP Site 323-U1342 Aiello, Ivano W Knudson, Karla P Ravelo, Ana Christina Drake, Michelle K MEDIAN LATITUDE: 54.828337 * MEDIAN LONGITUDE: 176.916882 * SOUTH-BOUND LATITUDE: 54.828312 * WEST-BOUND LONGITUDE: 176.916712 * NORTH-BOUND LATITUDE: 54.828362 * EAST-BOUND LONGITUDE: 176.917053 * MINIMUM ELEVATION: -818.8 m * MAXIMUM ELEVATION: -818.2 m text/tab-separated-values, 906 data points https://doi.pangaea.de/10.1594/PANGAEA.933699 en eng PANGAEA Knudson, Karla P; Ravelo, Ana Christina; Aiello, Ivano W; Knudson, C P; Drake, Michelle K; Sakamoto, Tatsuhiko (accepted): Causes and Timing of Subarctic Pacific Hypoxia. Science Advances https://doi.pangaea.de/10.1594/PANGAEA.933699 CC-BY-4.0: Creative Commons Attribution 4.0 International (License comes into effect after moratorium ends) Access constraints: access rights needed info:eu-repo/semantics/restrictedAccess 323-U1342C 323-U1342D AGE Bering Sea Bering Sea Paleoceanography Calcareous spicules Clay Coccolithophores Coccoliths Depth bottom/max top/min diatoms centrales pennales DRILL Drilling/drill rig Event label Exp323 Foraminifera grain counts iron fertilization Joides Resolution laminated North Pacific Opaque minerals Radiolarians Run Sample code/label Sample mass Sample type sediments see abstract Siliciclastics Silicoflagellates Size fraction Size fraction mode size smear slide sponge spicules Standard deviation Total Volcanic components dataset ftpangaea 2024-07-24T02:31:34Z Here we present new grain count data from from Integrated Ocean Drilling Program (IODP) Expedition 323 Site U1342 Holes A, C, and D. New records of sediment composition from laminated and non-laminated were determined from smear slide (quantitative grain counts) and particle size analyses. A subset of samples from three laminated intervals (672-697 ka, 826-836 ka, and 847-851 ka) and four adjacent massive intervals (668-671 ka, 822-825 ka, 803-845 ka, and 853-856 ka) were selected for analyses. Sediment smear slides were examined with a transmitted light petrographic microscope equipped with a standard eyepiece micrometer. Biogenic (pennate and centric diatoms, silicoflagellates, sponge spicules, foraminifers, and coccolithophores), mineral (clay minerals, silt- to sand-size siliciclastics), and volcaniclastic components were identified and their percentage abundances were visually determined under a petrographic microscope using a 40X objective and 10X eyepiece. For each sample, 3 counts were done on different parts of a smear slide using a random walk, and the average value of the 3 counts was used. Particle size analyses on the same samples were carried out with a Beckman-Coulter LS 13 320 laser particle size analyzer (LPSA) attached to an aqueous module equipped with a pump and a built-in ultrasound unit. Size distributions were analyzed from 0.04 µm to 2 mm. Measurements of such a wide particle size range are possible because the particle sizer is composed of two units: a laser beam for conventional (Fraunhofer) diffraction (from 0.4 µm to 2 mm) and a polarized intensity differential scatter (PIDS) unit, which measures particles based on the Mie theory of light scattering (0.04 µm). The samples for the analyses were subsampled and dispersed in the deionized water of the aqueous module of the particle sizer until obscuration values of 10%–15% and PIDS obscuration values of 48%–52% were obtained. The optical model chosen for the grain size determination is the default Fraunhofer model, based on the Fraunhofer ... Dataset Bering Sea PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(176.916712,176.917053,54.828362,54.828312)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 323-U1342C
323-U1342D
AGE
Bering Sea
Bering Sea Paleoceanography
Calcareous spicules
Clay
Coccolithophores
Coccoliths
Depth
bottom/max
top/min
diatoms
centrales
pennales
DRILL
Drilling/drill rig
Event label
Exp323
Foraminifera
grain counts
iron fertilization
Joides Resolution
laminated
North Pacific
Opaque minerals
Radiolarians
Run
Sample code/label
Sample mass
Sample type
sediments
see abstract
Siliciclastics
Silicoflagellates
Size fraction
Size fraction mode size
smear slide
sponge spicules
Standard deviation
Total
Volcanic components
spellingShingle 323-U1342C
323-U1342D
AGE
Bering Sea
Bering Sea Paleoceanography
Calcareous spicules
Clay
Coccolithophores
Coccoliths
Depth
bottom/max
top/min
diatoms
centrales
pennales
DRILL
Drilling/drill rig
Event label
Exp323
Foraminifera
grain counts
iron fertilization
Joides Resolution
laminated
North Pacific
Opaque minerals
Radiolarians
Run
Sample code/label
Sample mass
Sample type
sediments
see abstract
Siliciclastics
Silicoflagellates
Size fraction
Size fraction mode size
smear slide
sponge spicules
Standard deviation
Total
Volcanic components
Aiello, Ivano W
Knudson, Karla P
Ravelo, Ana Christina
Drake, Michelle K
Smear slide grain counts from IODP Site 323-U1342
topic_facet 323-U1342C
323-U1342D
AGE
Bering Sea
Bering Sea Paleoceanography
Calcareous spicules
Clay
Coccolithophores
Coccoliths
Depth
bottom/max
top/min
diatoms
centrales
pennales
DRILL
Drilling/drill rig
Event label
Exp323
Foraminifera
grain counts
iron fertilization
Joides Resolution
laminated
North Pacific
Opaque minerals
Radiolarians
Run
Sample code/label
Sample mass
Sample type
sediments
see abstract
Siliciclastics
Silicoflagellates
Size fraction
Size fraction mode size
smear slide
sponge spicules
Standard deviation
Total
Volcanic components
description Here we present new grain count data from from Integrated Ocean Drilling Program (IODP) Expedition 323 Site U1342 Holes A, C, and D. New records of sediment composition from laminated and non-laminated were determined from smear slide (quantitative grain counts) and particle size analyses. A subset of samples from three laminated intervals (672-697 ka, 826-836 ka, and 847-851 ka) and four adjacent massive intervals (668-671 ka, 822-825 ka, 803-845 ka, and 853-856 ka) were selected for analyses. Sediment smear slides were examined with a transmitted light petrographic microscope equipped with a standard eyepiece micrometer. Biogenic (pennate and centric diatoms, silicoflagellates, sponge spicules, foraminifers, and coccolithophores), mineral (clay minerals, silt- to sand-size siliciclastics), and volcaniclastic components were identified and their percentage abundances were visually determined under a petrographic microscope using a 40X objective and 10X eyepiece. For each sample, 3 counts were done on different parts of a smear slide using a random walk, and the average value of the 3 counts was used. Particle size analyses on the same samples were carried out with a Beckman-Coulter LS 13 320 laser particle size analyzer (LPSA) attached to an aqueous module equipped with a pump and a built-in ultrasound unit. Size distributions were analyzed from 0.04 µm to 2 mm. Measurements of such a wide particle size range are possible because the particle sizer is composed of two units: a laser beam for conventional (Fraunhofer) diffraction (from 0.4 µm to 2 mm) and a polarized intensity differential scatter (PIDS) unit, which measures particles based on the Mie theory of light scattering (0.04 µm). The samples for the analyses were subsampled and dispersed in the deionized water of the aqueous module of the particle sizer until obscuration values of 10%–15% and PIDS obscuration values of 48%–52% were obtained. The optical model chosen for the grain size determination is the default Fraunhofer model, based on the Fraunhofer ...
format Dataset
author Aiello, Ivano W
Knudson, Karla P
Ravelo, Ana Christina
Drake, Michelle K
author_facet Aiello, Ivano W
Knudson, Karla P
Ravelo, Ana Christina
Drake, Michelle K
author_sort Aiello, Ivano W
title Smear slide grain counts from IODP Site 323-U1342
title_short Smear slide grain counts from IODP Site 323-U1342
title_full Smear slide grain counts from IODP Site 323-U1342
title_fullStr Smear slide grain counts from IODP Site 323-U1342
title_full_unstemmed Smear slide grain counts from IODP Site 323-U1342
title_sort smear slide grain counts from iodp site 323-u1342
publisher PANGAEA
url https://doi.pangaea.de/10.1594/PANGAEA.933699
op_coverage MEDIAN LATITUDE: 54.828337 * MEDIAN LONGITUDE: 176.916882 * SOUTH-BOUND LATITUDE: 54.828312 * WEST-BOUND LONGITUDE: 176.916712 * NORTH-BOUND LATITUDE: 54.828362 * EAST-BOUND LONGITUDE: 176.917053 * MINIMUM ELEVATION: -818.8 m * MAXIMUM ELEVATION: -818.2 m
long_lat ENVELOPE(176.916712,176.917053,54.828362,54.828312)
genre Bering Sea
genre_facet Bering Sea
op_relation Knudson, Karla P; Ravelo, Ana Christina; Aiello, Ivano W; Knudson, C P; Drake, Michelle K; Sakamoto, Tatsuhiko (accepted): Causes and Timing of Subarctic Pacific Hypoxia. Science Advances
https://doi.pangaea.de/10.1594/PANGAEA.933699
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International (License comes into effect after moratorium ends)
Access constraints: access rights needed
info:eu-repo/semantics/restrictedAccess
_version_ 1810436705045446656