GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka BP)

We present continuous records of 1 cm resolved sodium, sulfur, non-sea-salt sulfur, size-resolved insoluble particle concentrations and liquid conductivity using a Continuous Flow Analysis (CFA) system (McConnell et al., 2017) from the Greenland Ice Sheet Project Two (GISP2; 72.97°N, 38.80°W) ice co...

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Bibliographic Details
Main Authors: Sigl, Michael, McConnell, Joseph R, Chellman, Nathan J
Format: Dataset
Language:English
Published: PANGAEA 2023
Subjects:
AGE
CFA
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.962783
https://doi.org/10.1594/PANGAEA.962783
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.962783
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Accumulation rate in ice equivalent per year
AGE
Calculated
running median
CFA
Conductivity
electrolytic
Continuous Flow Analysis
Corrected
Deposition of sulfate
volcanic
cumulative
DEPTH
ice/snow
DRILL
Drilling/drill rig
dust
insoluble
GISP
GISP2
Greenland
Ice core
Sampling/drilling ice
Sodium
Sulfate
background
Sulfur
non-sea-salt
Volcanic aerosol
volcanic eruption
spellingShingle Accumulation rate in ice equivalent per year
AGE
Calculated
running median
CFA
Conductivity
electrolytic
Continuous Flow Analysis
Corrected
Deposition of sulfate
volcanic
cumulative
DEPTH
ice/snow
DRILL
Drilling/drill rig
dust
insoluble
GISP
GISP2
Greenland
Ice core
Sampling/drilling ice
Sodium
Sulfate
background
Sulfur
non-sea-salt
Volcanic aerosol
volcanic eruption
Sigl, Michael
McConnell, Joseph R
Chellman, Nathan J
GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka BP)
topic_facet Accumulation rate in ice equivalent per year
AGE
Calculated
running median
CFA
Conductivity
electrolytic
Continuous Flow Analysis
Corrected
Deposition of sulfate
volcanic
cumulative
DEPTH
ice/snow
DRILL
Drilling/drill rig
dust
insoluble
GISP
GISP2
Greenland
Ice core
Sampling/drilling ice
Sodium
Sulfate
background
Sulfur
non-sea-salt
Volcanic aerosol
volcanic eruption
description We present continuous records of 1 cm resolved sodium, sulfur, non-sea-salt sulfur, size-resolved insoluble particle concentrations and liquid conductivity using a Continuous Flow Analysis (CFA) system (McConnell et al., 2017) from the Greenland Ice Sheet Project Two (GISP2; 72.97°N, 38.80°W) ice core and estimated volcanic sulfate mass depositions for the depth interval 2635-2638 m (equivalent to an age of c. 80 ka BP on GICC05modelext (Seierstad et al., 2014) and 79.5 ka BP on AICC2012 (Veres et al., 2013). The reconstruction is based on sulfur measurements employing high-resolution continuous flow analysis coupled to inductively coupled plasma mass spectrometry performed at the Desert Research Institute (Reno, NV, USA) under (class 100) cleanroom conditions. Volcanic eruptions are detected when annual sulfur concentrations exceeded the background concentrations + 4 times the median of the absolute deviation. Background concentrations are estimated using a 101-point running median. Volcanic sulfate deposition rates are calculated by subtracting the background concentrations from total sulfate equivalent (i.e. sulfur x 3) concentrations using thinning corrected estimates of mean ice accumulation rates at the ice-core site.
format Dataset
author Sigl, Michael
McConnell, Joseph R
Chellman, Nathan J
author_facet Sigl, Michael
McConnell, Joseph R
Chellman, Nathan J
author_sort Sigl, Michael
title GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka BP)
title_short GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka BP)
title_full GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka BP)
title_fullStr GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka BP)
title_full_unstemmed GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka BP)
title_sort gisp2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka bp)
publisher PANGAEA
publishDate 2023
url https://doi.pangaea.de/10.1594/PANGAEA.962783
https://doi.org/10.1594/PANGAEA.962783
op_coverage LATITUDE: 72.970000 * LONGITUDE: -38.800000 * DATE/TIME START: 1990-01-01T00:39:00 * DATE/TIME END: 1990-01-01T00:39:00 * MINIMUM DEPTH, ice/snow: 2635.005 m * MAXIMUM DEPTH, ice/snow: 2637.965 m
long_lat ENVELOPE(-117.003,-117.003,56.000,56.000)
ENVELOPE(-38.800000,-38.800000,72.970000,72.970000)
geographic Greenland
Reno
geographic_facet Greenland
Reno
genre GISP
Greenland
Greenland ice core
Greenland Ice Sheet Project
ice core
Ice Sheet
genre_facet GISP
Greenland
Greenland ice core
Greenland Ice Sheet Project
ice core
Ice Sheet
op_relation Innes, Helen M; et al. (in review): Precise new date for the Los Chocoyos supereruption precludes millennial-scale climatic impact.
McConnell, Joseph R; Burke, Andrea; Dunbar, Nelia W; Köhler, Peter; Thomas, Jennie L; Arienzo, Monica M; Chellman, Nathan J; Maselli, Olivia J; Sigl, Michael; Adkins, Jess F; Baggenstos, Daniel; Burkhart, John F; Brook, Edward J; Buizert, Christo; Cole-Dai, Jihong; Fudge, Tyler J; Knorr, Gregor; Graf, Hans-Friedrich; Grieman, Mackenzie M; Iverson, Nels; McGwire, Kenneth C; Mulvaney, Robert; Paris, Guillaume; Rhodes, Rachael H; Saltzman, Eric S; Severinghaus, Jeffrey P; Steffensen, Jørgen Peder; Taylor, Kendrick C; Winckler, Gisela (2017): Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion. Proceedings of the National Academy of Sciences, 114(38), 10035-10040, https://doi.org/10.1073/pnas.1705595114
Seierstad, Inger K; Abbott, Peter M; Bigler, Matthias; Blunier, Thomas; Bourne, Anna J; Brook, Edward J; Buchardt, Susanne L; Buizert, Christo; Clausen, Henrik Brink; Cook, Eliza; Dahl-Jensen, Dorthe; Davies, Siwan M; Guillevic, Myriam; Johnsen, Sigfús Jóhann; Pedersen, Desirée S; Popp, Trevor J; Rasmussen, Sune Olander; Severinghaus, Jeffrey P; Svensson, Anders M; Vinther, Bo Møllesøe (2014): Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint. Quaternary Science Reviews, 106, 29-46, https://doi.org/10.1016/j.quascirev.2014.10.032
Veres, Daniel; Bazin, Lucie; Landais, Amaëlle; Toyé Mahamadou Kele, H; Lemieux-Dudon, Bénédicte; Parrenin, Frédéric; Martinerie, Patricia; Blayo, Eric; Blunier, Thomas; Capron, Emilie; Chappellaz, Jérôme A; Rasmussen, Sune Olander; Severi, Mirko; Svensson, Anders M; Vinther, Bo Møllesøe; Wolff, Eric William (2013): The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years. Climate of the Past, 9(4), 1733-1748, https://doi.org/10.5194/cp-9-1733-2013
https://doi.pangaea.de/10.1594/PANGAEA.962783
https://doi.org/10.1594/PANGAEA.962783
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.96278310.1073/pnas.170559511410.1016/j.quascirev.2014.10.03210.5194/cp-9-1733-2013
_version_ 1813448021123268608
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.962783 2024-10-20T14:08:49+00:00 GISP2 ice-core volcanic sulfate concentration and deposition between 2635 and 2638 m depth (c. 80 ka BP) Sigl, Michael McConnell, Joseph R Chellman, Nathan J LATITUDE: 72.970000 * LONGITUDE: -38.800000 * DATE/TIME START: 1990-01-01T00:39:00 * DATE/TIME END: 1990-01-01T00:39:00 * MINIMUM DEPTH, ice/snow: 2635.005 m * MAXIMUM DEPTH, ice/snow: 2637.965 m 2023 text/tab-separated-values, 3270 data points https://doi.pangaea.de/10.1594/PANGAEA.962783 https://doi.org/10.1594/PANGAEA.962783 en eng PANGAEA Innes, Helen M; et al. (in review): Precise new date for the Los Chocoyos supereruption precludes millennial-scale climatic impact. McConnell, Joseph R; Burke, Andrea; Dunbar, Nelia W; Köhler, Peter; Thomas, Jennie L; Arienzo, Monica M; Chellman, Nathan J; Maselli, Olivia J; Sigl, Michael; Adkins, Jess F; Baggenstos, Daniel; Burkhart, John F; Brook, Edward J; Buizert, Christo; Cole-Dai, Jihong; Fudge, Tyler J; Knorr, Gregor; Graf, Hans-Friedrich; Grieman, Mackenzie M; Iverson, Nels; McGwire, Kenneth C; Mulvaney, Robert; Paris, Guillaume; Rhodes, Rachael H; Saltzman, Eric S; Severinghaus, Jeffrey P; Steffensen, Jørgen Peder; Taylor, Kendrick C; Winckler, Gisela (2017): Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion. Proceedings of the National Academy of Sciences, 114(38), 10035-10040, https://doi.org/10.1073/pnas.1705595114 Seierstad, Inger K; Abbott, Peter M; Bigler, Matthias; Blunier, Thomas; Bourne, Anna J; Brook, Edward J; Buchardt, Susanne L; Buizert, Christo; Clausen, Henrik Brink; Cook, Eliza; Dahl-Jensen, Dorthe; Davies, Siwan M; Guillevic, Myriam; Johnsen, Sigfús Jóhann; Pedersen, Desirée S; Popp, Trevor J; Rasmussen, Sune Olander; Severinghaus, Jeffrey P; Svensson, Anders M; Vinther, Bo Møllesøe (2014): Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint. Quaternary Science Reviews, 106, 29-46, https://doi.org/10.1016/j.quascirev.2014.10.032 Veres, Daniel; Bazin, Lucie; Landais, Amaëlle; Toyé Mahamadou Kele, H; Lemieux-Dudon, Bénédicte; Parrenin, Frédéric; Martinerie, Patricia; Blayo, Eric; Blunier, Thomas; Capron, Emilie; Chappellaz, Jérôme A; Rasmussen, Sune Olander; Severi, Mirko; Svensson, Anders M; Vinther, Bo Møllesøe; Wolff, Eric William (2013): The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years. Climate of the Past, 9(4), 1733-1748, https://doi.org/10.5194/cp-9-1733-2013 https://doi.pangaea.de/10.1594/PANGAEA.962783 https://doi.org/10.1594/PANGAEA.962783 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Accumulation rate in ice equivalent per year AGE Calculated running median CFA Conductivity electrolytic Continuous Flow Analysis Corrected Deposition of sulfate volcanic cumulative DEPTH ice/snow DRILL Drilling/drill rig dust insoluble GISP GISP2 Greenland Ice core Sampling/drilling ice Sodium Sulfate background Sulfur non-sea-salt Volcanic aerosol volcanic eruption dataset 2023 ftpangaea https://doi.org/10.1594/PANGAEA.96278310.1073/pnas.170559511410.1016/j.quascirev.2014.10.03210.5194/cp-9-1733-2013 2024-09-25T00:03:38Z We present continuous records of 1 cm resolved sodium, sulfur, non-sea-salt sulfur, size-resolved insoluble particle concentrations and liquid conductivity using a Continuous Flow Analysis (CFA) system (McConnell et al., 2017) from the Greenland Ice Sheet Project Two (GISP2; 72.97°N, 38.80°W) ice core and estimated volcanic sulfate mass depositions for the depth interval 2635-2638 m (equivalent to an age of c. 80 ka BP on GICC05modelext (Seierstad et al., 2014) and 79.5 ka BP on AICC2012 (Veres et al., 2013). The reconstruction is based on sulfur measurements employing high-resolution continuous flow analysis coupled to inductively coupled plasma mass spectrometry performed at the Desert Research Institute (Reno, NV, USA) under (class 100) cleanroom conditions. Volcanic eruptions are detected when annual sulfur concentrations exceeded the background concentrations + 4 times the median of the absolute deviation. Background concentrations are estimated using a 101-point running median. Volcanic sulfate deposition rates are calculated by subtracting the background concentrations from total sulfate equivalent (i.e. sulfur x 3) concentrations using thinning corrected estimates of mean ice accumulation rates at the ice-core site. Dataset GISP Greenland Greenland ice core Greenland Ice Sheet Project ice core Ice Sheet PANGAEA - Data Publisher for Earth & Environmental Science Greenland Reno ENVELOPE(-117.003,-117.003,56.000,56.000) ENVELOPE(-38.800000,-38.800000,72.970000,72.970000)