TOC, TN, and sedimentary d15N and δ¹³C ratios of sediment core SO201-2-85
We present high-resolution records of sedimentary nitrogen (d15Nbulk) and carbon isotope ratios (d13Cbulk) from piston core SO201-2-85KL located in the western Bering Sea. The records reflect changes in surface nitrate utilization and terrestrial organic matter contribution in submillennial resoluti...
Main Authors: | , , , , , , |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2016
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.807383 https://doi.org/10.1594/PANGAEA.807383 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.807383 |
---|---|
record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AGE Carbon organic total Comment DEPTH sediment/rock Element analyser isotope ratio mass spectrometer (EA-IRMS) KALMAR II Nitrogen PC Piston corer Shirshov Ridge SO201/2 SO201-2-85 Sonne δ13C organic matter δ15N |
spellingShingle |
AGE Carbon organic total Comment DEPTH sediment/rock Element analyser isotope ratio mass spectrometer (EA-IRMS) KALMAR II Nitrogen PC Piston corer Shirshov Ridge SO201/2 SO201-2-85 Sonne δ13C organic matter δ15N Riethdorf, Jan-Rainer Thibodeau, Benoit Ikehara, Minoru Nürnberg, Dirk Max, Lars Tiedemann, Ralf Yokoyama, Yusuke TOC, TN, and sedimentary d15N and δ¹³C ratios of sediment core SO201-2-85 |
topic_facet |
AGE Carbon organic total Comment DEPTH sediment/rock Element analyser isotope ratio mass spectrometer (EA-IRMS) KALMAR II Nitrogen PC Piston corer Shirshov Ridge SO201/2 SO201-2-85 Sonne δ13C organic matter δ15N |
description |
We present high-resolution records of sedimentary nitrogen (d15Nbulk) and carbon isotope ratios (d13Cbulk) from piston core SO201-2-85KL located in the western Bering Sea. The records reflect changes in surface nitrate utilization and terrestrial organic matter contribution in submillennial resolution that span the last 180 kyr. The d15Nbulk record is characterized by a minimum during the penultimate interglacial indicating low nitrate utilization (~62-80%) despite the relatively high export production inferred from opal concentrations along with a significant reduction in the terrestrial organic matter fraction (mterr). This suggests that the consumption of the nitrate pool at our site was incomplete and even more reduced than today (~84%). d15Nbulk increases from Marine Isotope Stage (MIS) 5.4 and culminates during the Last Glacial Maximum, which indicates that nitrate utilization in the Bering Sea was raised during cold intervals (MIS 5.4, 5.2, 4) and almost complete during MIS 3 and 2 (~93-100%). This is in agreement with previous hypotheses suggesting that stronger glacial stratification reduced the nutrient supply from the subeuphotic zone, thereby increasing the iron-to-nutrient ratio and therefore the nitrate utilization in the mixed surface layer. Large variations in d15Nbulk were also recorded from 180 to 130 ka BP (MIS 6), indicating a potential link to insolation and sea-level forcing and its related feedbacks. Millennial-scale oscillations were observed in d15Nbulk and d13Cbulk that might be related to Greenland interstadials. |
format |
Dataset |
author |
Riethdorf, Jan-Rainer Thibodeau, Benoit Ikehara, Minoru Nürnberg, Dirk Max, Lars Tiedemann, Ralf Yokoyama, Yusuke |
author_facet |
Riethdorf, Jan-Rainer Thibodeau, Benoit Ikehara, Minoru Nürnberg, Dirk Max, Lars Tiedemann, Ralf Yokoyama, Yusuke |
author_sort |
Riethdorf, Jan-Rainer |
title |
TOC, TN, and sedimentary d15N and δ¹³C ratios of sediment core SO201-2-85 |
title_short |
TOC, TN, and sedimentary d15N and δ¹³C ratios of sediment core SO201-2-85 |
title_full |
TOC, TN, and sedimentary d15N and δ¹³C ratios of sediment core SO201-2-85 |
title_fullStr |
TOC, TN, and sedimentary d15N and δ¹³C ratios of sediment core SO201-2-85 |
title_full_unstemmed |
TOC, TN, and sedimentary d15N and δ¹³C ratios of sediment core SO201-2-85 |
title_sort |
toc, tn, and sedimentary d15n and δ¹³c ratios of sediment core so201-2-85 |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.807383 https://doi.org/10.1594/PANGAEA.807383 |
op_coverage |
LATITUDE: 57.505000 * LONGITUDE: 170.413167 * DATE/TIME START: 2009-09-21T08:05:00 * DATE/TIME END: 2009-09-21T08:49:00 * MINIMUM DEPTH, sediment/rock: 0.165 m * MAXIMUM DEPTH, sediment/rock: 18.115 m |
long_lat |
ENVELOPE(170.413167,170.413167,57.505000,57.505000) |
genre |
Bering Sea Greenland |
genre_facet |
Bering Sea Greenland |
op_source |
Supplement to: Riethdorf, Jan-Rainer; Thibodeau, Benoit; Ikehara, Minoru; Nürnberg, Dirk; Max, Lars; Tiedemann, Ralf; Yokoyama, Yusuke (2016): Surface nitrate utilization in the Bering sea since 180kA BP: Insight from sedimentary nitrogen isotopes. Deep Sea Research Part II: Topical Studies in Oceanography, 125-126, 163-176, https://doi.org/10.1016/j.dsr2.2015.03.007 |
op_relation |
Max, Lars; Riethdorf, Jan-Rainer; Tiedemann, Ralf; Smirnova, Maria; Lembke-Jene, Lester; Fahl, Kirsten; Nürnberg, Dirk; Matul, Alexander G; Mollenhauer, Gesine (2012): Sea surface temperature variability and sea-ice extent in the subarctic northwest Pacific during the past 15,000 years. Paleoceanography, 27(3), PA3213, https://doi.org/10.1029/2012PA002292 Riethdorf, Jan-Rainer; Max, Lars; Nürnberg, Dirk; Lembke-Jene, Lester; Tiedemann, Ralf (2013): Deglacial development of (sub) sea surface temperature and salinity in the subarctic northwest Pacific: Implications for upper-ocean stratification. Paleoceanography, 28(1), 91-104, https://doi.org/10.1002/palo.20014 Riethdorf, Jan-Rainer; Nürnberg, Dirk; Max, Lars; Tiedemann, Ralf; Gorbarenko, Sergey A; Malakhov, Mikhail I (2013): Millennial-scale variability of marine productivity and terrigenous matter supply in the western Bering Sea over the past 180 kyr. Climate of the Past, 9(3), 1345-1373, https://doi.org/10.5194/cp-9-1345-2013 https://doi.pangaea.de/10.1594/PANGAEA.807383 https://doi.org/10.1594/PANGAEA.807383 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.80738310.1016/j.dsr2.2015.03.00710.1029/2012PA00229210.1002/palo.2001410.5194/cp-9-1345-2013 |
_version_ |
1810436673155104768 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.807383 2024-09-15T17:59:34+00:00 TOC, TN, and sedimentary d15N and δ¹³C ratios of sediment core SO201-2-85 Riethdorf, Jan-Rainer Thibodeau, Benoit Ikehara, Minoru Nürnberg, Dirk Max, Lars Tiedemann, Ralf Yokoyama, Yusuke LATITUDE: 57.505000 * LONGITUDE: 170.413167 * DATE/TIME START: 2009-09-21T08:05:00 * DATE/TIME END: 2009-09-21T08:49:00 * MINIMUM DEPTH, sediment/rock: 0.165 m * MAXIMUM DEPTH, sediment/rock: 18.115 m 2016 text/tab-separated-values, 1427 data points https://doi.pangaea.de/10.1594/PANGAEA.807383 https://doi.org/10.1594/PANGAEA.807383 en eng PANGAEA Max, Lars; Riethdorf, Jan-Rainer; Tiedemann, Ralf; Smirnova, Maria; Lembke-Jene, Lester; Fahl, Kirsten; Nürnberg, Dirk; Matul, Alexander G; Mollenhauer, Gesine (2012): Sea surface temperature variability and sea-ice extent in the subarctic northwest Pacific during the past 15,000 years. Paleoceanography, 27(3), PA3213, https://doi.org/10.1029/2012PA002292 Riethdorf, Jan-Rainer; Max, Lars; Nürnberg, Dirk; Lembke-Jene, Lester; Tiedemann, Ralf (2013): Deglacial development of (sub) sea surface temperature and salinity in the subarctic northwest Pacific: Implications for upper-ocean stratification. Paleoceanography, 28(1), 91-104, https://doi.org/10.1002/palo.20014 Riethdorf, Jan-Rainer; Nürnberg, Dirk; Max, Lars; Tiedemann, Ralf; Gorbarenko, Sergey A; Malakhov, Mikhail I (2013): Millennial-scale variability of marine productivity and terrigenous matter supply in the western Bering Sea over the past 180 kyr. Climate of the Past, 9(3), 1345-1373, https://doi.org/10.5194/cp-9-1345-2013 https://doi.pangaea.de/10.1594/PANGAEA.807383 https://doi.org/10.1594/PANGAEA.807383 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Riethdorf, Jan-Rainer; Thibodeau, Benoit; Ikehara, Minoru; Nürnberg, Dirk; Max, Lars; Tiedemann, Ralf; Yokoyama, Yusuke (2016): Surface nitrate utilization in the Bering sea since 180kA BP: Insight from sedimentary nitrogen isotopes. Deep Sea Research Part II: Topical Studies in Oceanography, 125-126, 163-176, https://doi.org/10.1016/j.dsr2.2015.03.007 AGE Carbon organic total Comment DEPTH sediment/rock Element analyser isotope ratio mass spectrometer (EA-IRMS) KALMAR II Nitrogen PC Piston corer Shirshov Ridge SO201/2 SO201-2-85 Sonne δ13C organic matter δ15N dataset 2016 ftpangaea https://doi.org/10.1594/PANGAEA.80738310.1016/j.dsr2.2015.03.00710.1029/2012PA00229210.1002/palo.2001410.5194/cp-9-1345-2013 2024-07-24T02:31:32Z We present high-resolution records of sedimentary nitrogen (d15Nbulk) and carbon isotope ratios (d13Cbulk) from piston core SO201-2-85KL located in the western Bering Sea. The records reflect changes in surface nitrate utilization and terrestrial organic matter contribution in submillennial resolution that span the last 180 kyr. The d15Nbulk record is characterized by a minimum during the penultimate interglacial indicating low nitrate utilization (~62-80%) despite the relatively high export production inferred from opal concentrations along with a significant reduction in the terrestrial organic matter fraction (mterr). This suggests that the consumption of the nitrate pool at our site was incomplete and even more reduced than today (~84%). d15Nbulk increases from Marine Isotope Stage (MIS) 5.4 and culminates during the Last Glacial Maximum, which indicates that nitrate utilization in the Bering Sea was raised during cold intervals (MIS 5.4, 5.2, 4) and almost complete during MIS 3 and 2 (~93-100%). This is in agreement with previous hypotheses suggesting that stronger glacial stratification reduced the nutrient supply from the subeuphotic zone, thereby increasing the iron-to-nutrient ratio and therefore the nitrate utilization in the mixed surface layer. Large variations in d15Nbulk were also recorded from 180 to 130 ka BP (MIS 6), indicating a potential link to insolation and sea-level forcing and its related feedbacks. Millennial-scale oscillations were observed in d15Nbulk and d13Cbulk that might be related to Greenland interstadials. Dataset Bering Sea Greenland PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(170.413167,170.413167,57.505000,57.505000) |