cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.816263
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 1998/1999

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816264
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 1999/2000

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816265
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2000/2001

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816266
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2001/2002

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816267
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2002/2003

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816268
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2003/2004

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816269
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2004/2005

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816270
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2005/2006

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816271
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2006/2007

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816272
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2007/2008

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816273
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2008/2009

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816274
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2009/2010

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816275
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2010/2011

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816276
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2011/2012

description: The glacier mass balance of Jamtalferner has been measured annually since 1988/1989 with the direct/glaciological method. Winter mass balance has been determined for 1 May in all years. The mass balance records are complemented by precipitation measurements at a gauge close to the glacier tongue and climate data recorded at the village of Galtür.
DOI: 10.1594/pangaea.816277
title: Elevation zones Jamtalferner, Silvretta, Austria, 1988/1989
DOI: 10.1594/pangaea.816278
title: Elevation zones Jamtalferner, Silvretta, Austria, 1989/1990
DOI: 10.1594/pangaea.816279
title: Elevation zones Jamtalferner, Silvretta, Austria, 1990/1991
DOI: 10.1594/pangaea.816280
title: Elevation zones Jamtalferner, Silvretta, Austria, 1991/1992
DOI: 10.1594/pangaea.816281
title: Elevation zones Jamtalferner, Silvretta, Austria, 1992/1993
DOI: 10.1594/pangaea.816282
title: Elevation zones Jamtalferner, Silvretta, Austria, 1993/1994
DOI: 10.1594/pangaea.816283
title: Elevation zones Jamtalferner, Silvretta, Austria, 1994/1995
DOI: 10.1594/pangaea.816284
title: Elevation zones Jamtalferner, Silvretta, Austria, 1995/1996
DOI: 10.1594/pangaea.816285
title: Elevation zones Jamtalferner, Silvretta, Austria, 1996/1997
DOI: 10.1594/pangaea.816286
title: Elevation zones Jamtalferner, Silvretta, Austria, 1997/1998
DOI: 10.1594/pangaea.816287
title: Elevation zones Jamtalferner, Silvretta, Austria, 1998/1999
DOI: 10.1594/pangaea.816288
title: Elevation zones Jamtalferner, Silvretta, Austria, 1999/2000
DOI: 10.1594/pangaea.816289
title: Elevation zones Jamtalferner, Silvretta, Austria, 2000/2001
DOI: 10.1594/pangaea.816290
title: Elevation zones Jamtalferner, Silvretta, Austria, 2001/2002
DOI: 10.1594/pangaea.816291
title: Elevation zones Jamtalferner, Silvretta, Austria, 2002/2003
DOI: 10.1594/pangaea.816292
title: Elevation zones Jamtalferner, Silvretta, Austria, 2003/2004
DOI: 10.1594/pangaea.816293
title: Elevation zones Jamtalferner, Silvretta, Austria, 2004/2005
DOI: 10.1594/pangaea.816294
title: Elevation zones Jamtalferner, Silvretta, Austria, 2005/2006
DOI: 10.1594/pangaea.816295
title: Elevation zones Jamtalferner, Silvretta, Austria, 2006/2007
DOI: 10.1594/pangaea.816296
title: Elevation zones Jamtalferner, Silvretta, Austria, 2007/2008
DOI: 10.1594/pangaea.816297
title: Elevation zones Jamtalferner, Silvretta, Austria, 2008/2009
DOI: 10.1594/pangaea.816298
title: Elevation zones Jamtalferner, Silvretta, Austria, 2009/2010
DOI: 10.1594/pangaea.816299
title: Elevation zones Jamtalferner, Silvretta, Austria, 2010/2011
DOI: 10.1594/pangaea.816300
title: Elevation zones Jamtalferner, Silvretta, Austria, 2011/2012
DOI: 10.1594/pangaea.824866
title: AICC2012 chronology for ice core EDML
DOI: 10.1594/pangaea.824867
title: AICC2012 chronology for ice core NGRIP
DOI: 10.1594/pangaea.824868
title: AICC2012 chronology for ice core TALDICE

description: Only build back to 150 ka. Do not use it prior to 150 ka.
DOI: 10.1594/pangaea.824869
title: AICC2012 chronology for ice core Vostok
DOI: 10.1594/pangaea.824884
title: Methane measured on ice core EDML on AICC2012 chronology
DOI: 10.1594/pangaea.824885
title: Methane measured on ice core NGRIP on AICC2012 chronology
DOI: 10.1594/pangaea.824887
title: Methane measured on ice core Vostok on AICC2012 chronology
DOI: 10.1594/pangaea.824888
title: delta 18O measured on ice core EDML on AICC2012 chronology

description: AGE = ice age
DOI: 10.1594/pangaea.824889
title: delta 18O measured on ice core NGRIP on AICC2012 chronology

description: AGE = ice age
DOI: 10.1594/pangaea.824890
title: delta 18O measured on ice core TALDICE on AICC2012 chronology

description: AGE = ice age
DOI: 10.1594/pangaea.824892
title: delta Deuterium measured on ice core Vostok on AICC2012 chronology

description: AGE = ice age
DOI: 10.1594/pangaea.824893
title: Carbon dioxide composite data on AICC2012 chronology
DOI: 10.1594/pangaea.833221
title: Glacier mass balance Hallstätter Gletscher, Dachstein, Austria, 2012/2013
DOI: 10.1594/pangaea.833222
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2012/2013
DOI: 10.1594/pangaea.833227
title: Elevation zones Hallstätter Gletscher, Dachstein, Austria, 2012/2013
DOI: 10.1594/pangaea.833269
title: Elevation zones Jamtalferner, Silvretta, Austria, 2012/2013
DOI: 10.1594/pangaea.849403
title: Age control points for IODP Site 339-U1389
DOI: 10.1594/pangaea.841719
title: Glacier mass balance Hallstätter Gletscher, Dachstein, Austria, 2013/2014
DOI: 10.1594/pangaea.841720
title: Elevation zones Hallstätter Gletscher, Dachstein, Austria, 2013/2014
DOI: 10.1594/pangaea.834699
title: (Table 2) Tie points of DSDP Site 94-609 and Greenland ice cores

description: DEPTH, sediment/rock gives meters below seafloor [mbsf]. The tie points to GISP2 used to produce the age model for Site 609 are shown at left (Bond et al., 1999). These data are presented graphically in Fig. 3 of Bond et al. (1999) but are not presented in table format as above. At right are our ties of the same depths in Site 609 to the NGRIP ice core. A 705-year shift to younger ages is required to align GICC05 and GICC05modelext time scales at 60 ka (Svensson et al., 2008). GISP2 depth 2465.9807: Based on the MS/94 age model for GISP2, which assigned ages of 53.22 ka and 53.5 ka to 2464 mand 2466 m, respectively, a tie point to a depth of exactly 2465.98071428571 m in GISP2 is required to obtain the age of 53.4973 ka that was assigned by Bond et al. (1999) to 347.5 cm in Site 609.
DOI: 10.1594/pangaea.839457
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2013/2014
DOI: 10.1594/pangaea.839458
title: Elevation zones Jamtalferner, Silvretta, Austria, 2013/2014
DOI: 10.1594/pangaea.859829
title: Glacier mass balance Hallstätter Gletscher, Dachstein, Austria, 2014/2015
DOI: 10.1594/pangaea.859833
title: Elevation zones Hallstätter Gletscher, Dachstein, Austria, 2014/2015
DOI: 10.1594/pangaea.859834
title: Elevation zones Jamtalferner, Silvretta, Austria, 2014/2015
DOI: 10.1594/pangaea.859837
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2014/2015
DOI: 10.1594/pangaea.860381
title: Population genetic and dispersal modeling data for Bathymodiolus mussels from the Mid-Atlantic Ridge

description: The zip folder comprises a text file and a gzipped tar archive. 1) The text file contains individual genotype data for 90 SNPs, 9 microsatellites and the mitochondrial ND4 gene that were determined in deep-sea hydrothermal vent mussels from the Mid-Atlantic Ridge (genus Bathymodiolus). Mussel specimens are grouped according to the population (pop)/location from which they have been sampled (first column). The remaining columns contain the respective allele/haplotype codes for the different genetic loci (names in the header line). The data file is in CONVERT format and can be directly transformed into different input files for population genetic statistics. 2) The tar archive contains NetCDF files with larval dispersal probabilities for simulated annual larval releases between 1998 and 2007. For each simulated vent location (Menez Gwen, Lucky Strike, Rainbow, Vent 1-10) two NetCDF files are given, one for an assumed pelagic larval duration of 1 year and the other one for an assumed pelagic larval duration of 6 months (6m).
description: Supplement to: Breusing, Corinna; Biastoch, Arne; Drews, Annika; Metaxas, Anna; Jollivet, Didier; Vrijenhoek, Robert C; Bayer, Till; Melzner, Frank; Sayavedra, Lizbeth; Petersen, Jillian M; Dubilier, Nicole; Schilhabel, Markus B; Rosenstiel, Philip; Reusch, Thorsten B H (2016): Biophysical and Population Genetic Models Predict the Presence of “Phantom” Stepping Stones Connecting Mid-Atlantic Ridge Vent Ecosystems. Current Biology, 26, 1-11
DOI: 10.1594/pangaea.871563
title: 200 and 1000 y low pass filtered firn temperature reconstruction based on diffusion length history for ice core NorthGRIP
DOI: 10.1594/pangaea.871564
title: Accumulation reconstruction using a DJ model for the NorthGRIP site
DOI: 10.1594/pangaea.871565
title: Accumulation reconstruction using a DJ model for the NorthGRIP site, proposed
DOI: 10.1594/pangaea.872451
title: High-resolution 10Be concentrations in the EDML ice core
DOI: 10.1594/pangaea.872452
title: High-resolution 10Be concentrations in the NGRIP ice core
DOI: 10.1594/pangaea.872453
title: High-resolution 10Be concentrations and dD in the VOSTOK 5G ice core
DOI: 10.1594/pangaea.875711
title: Major elemental concentrations from NGRIP ice core across the interstadial period GI-21.2

description: Several abrupt shifts from periods of extreme cold (Greenland stadials, GS) to relatively warmer conditions (Greenland interstadials, GI) called Dansgaard-Oeschger events are recorded in the Greenland ice cores. Using cryo-cell UV-laser-ablation inductively-coupled-plasma mass spectrometry (UV-LA-ICPMS), we analysed a 2.85 m NGRIP ice core section (~ 250 years; 2691.50–2688.65 m depth) across the transitions of GI-21.2, a short-lived interstadial prior to interstadial GI-21.1 (GI-21.2: 84.87–85.09 ka b2k). GI-21.2 is a ~100-year-long period with d18O values 3–4 per mil higher than the following ~200 years of stadial conditions (GS-21.2), which precede the major GI-21.1 warming. We report concentrations of "major" elements indicative of dust and/or sea salt (Na, Fe, Al, Ca, Mg) at a spatial resolution of ~ 200 µm, while maintaining detection limits in the low-ppb range, thereby achieving sub-annual time resolution even in deep NGRIP ice. We present an improved external calibration and quantification procedure using a set of five ice standards made from aqueous (international) standard solutions. Our results show that element concentrations decrease drastically (more than tenfold) at the warming onset of GI-21.2 at the scale of a single year, followed by relatively low concentrations characterizing the interstadial part before gradually reaching again typical stadial values.
description: Supplement to: Della Lunga, Damiano; Müller, Wolfgang; Rasmussen, Sune Olander; Svensson, Anders M; Vallelonga, Paul T (2017): Calibrated cryo-cell UV-LA-ICPMS elemental concentrations from the NGRIP ice core reveal abrupt, sub-annual variability in dust across the GI-21.2 interstadial period. The Cryosphere, 11(3), 1297-1309
DOI: 10.1594/pangaea.886085
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2015/2016
DOI: 10.1594/pangaea.886086
title: Glacier mass balance Hallstätter Gletscher, Dachstein, Austria, 2016/2017
DOI: 10.1594/pangaea.886037
title: Water stable isotope record of ice core Dome Fuji

description: Whereas ice cores from high-accumulation sites in coastal Antarctica clearly demonstrate annual layering, it is debated whether a seasonal signal is also preserved in ice cores from lower-accumulation sites further inland and particularly on the East Antarctic Plateau. In this study, we examine 5 m of early Holocene ice from the Dome Fuji (DF) ice core at a high temporal resolution by continuous flow analysis. The ice was continuously analysed for concentrations of dust, sodium, ammonium, liquid conductivity, and water isotopic composition. Furthermore, a dielectric profiling was performed on the solid ice. In most of the analysed ice, the multi-parameter impurity data set appears to resolve the seasonal variability although the identification of annual layers is not always unambiguous. The study thus provides information on the snow accumulation process in central East Antarctica. A layer counting based on the same principles as those previously applied to the NGRIP (North Greenland Ice core Project) and the Antarctic EPICA (European Project for Ice Coring in Antarctica) Dronning Maud Land (EDML) ice cores leads to a mean annual layer thickness for the DF ice of 3.0 ± 0.3 cm that compares well to existing estimates. The measured DF section is linked to the EDML ice core through a characteristic pattern of three significant acidity peaks that are present in both cores. The corresponding section of the EDML ice core has recently been dated by annual layer counting and the number of years identified independently in the two cores agree within error estimates. We therefore conclude that, to first order, the annual signal is preserved in this section of the DF core. This case study demonstrates the feasibility of determining annually deposited strata on the central East Antarctic Plateau. It also opens the possibility of resolving annual layers in the Eemian section of Antarctic ice cores where the accumulation is estimated to have been greater than in the Holocene.
description: Dome Fuji CFA measurements coupled with a Picarro 1102. The age in this depth region is around 9.6 kab2k.
description: Supplement to: Svensson, Anders M; Fujita, Shuji; Bigler, Matthias; Braun, M; Dallmayr, Remi; Gkinis, Vasileios; Goto-Azuma, Kumiko; Hirabayashi, Motohiro; Kawamura, K; Kipfstuhl, Sepp; Kjær, Helle Astrid; Popp, Trevor; Simonsen, Marius; Steffensen, Jørgen Peder; Vallelonga, Paul T; Vinther, Bo Møllesøe (2015): On the occurrence of annual layers in Dome Fuji ice core early Holocene ice. Climate of the Past, 11(9), 1127-1137
DOI: 10.1594/pangaea.886087
title: Glacier mass balance Jamtalferner, Silvretta, Austria, 2016/2017
DOI: 10.1594/pangaea.886038
title: Water stable isotope record of ice core GRIP (early Holocene)

description: Measured discretely with a Picarro L2130 with a resolution of 2.5 cm. An early Holocene section with an age around 9.4 kab2k.
DOI: 10.1594/pangaea.886039
title: Water stable isotope record of ice core GRIP (late Holocene)

description: Measured discretely with a Picarro L2130 with a resolution of 2.5 cm. A late Holocene section with an age around 2.4 kab2k.
DOI: 10.1594/pangaea.886040
title: Water stable isotope record of ice core GRIP (mid Holocene)

description: Measured discretely with a Picarro L2130 with a resolution of 2.5 cm. A mid Holocene section with an age around 3.7 kab2k.
DOI: 10.1594/pangaea.886043
title: Water stable isotope record of ice core NEEM (top section)

description: Measured discretely with a Picarro L2120 with a resolution of 2.5 cm.
DOI: 10.1594/pangaea.886044
title: Water stable isotope record of ice cores NGRIP I and II

description: A high resolution (0.05 m) water isotopic record (d18O) is available from the NorthGRIP ice core. In this study we look into the water isotope diffusion history as estimated by the spectral characteristics of the d18O time series covering the last 16,000 years. The diffusion of water vapor in the porous medium of the firn pack attenuates the initial isotopic signal, predominantly having an impact on the high frequency components of the power spectrum. Higher temperatures induce higher rates of smoothing and thus the signal can be used as a firn paleothermometer. We use a water isotope diffusion model coupled to a steady-state densification model in order to infer the temperature signal from the site, assuming the accumulation and strain rate history as estimated using the GICC05 layer counted chronology and a Dansgaard-Johnsen ice flow model. The temperature reconstruction accurately captures the timing and magnitude of the Bølling-Allerød and Younger Dryas transitions. A Holocene climatic optimum is seen between 7 and 9 ky b2k with an apparent cooling trend thereafter. Our temperature estimate for the Holocene climatic optimum, points to a necessary adjustment of the ice thinning function indicating that the ice flow model overestimates past accumulation rates by about 10% at 8 ky b2k. This result, is supported by recent gas isotopic fractionation studies proposing a similar reduction for glacial conditions. Finally, the record presents a climatic variability over the Holocene spanning millennial and centennial scales with a profound cooling occurring at approximately 4000 years b2k. The new reconstruction technique is able to provide past temperature estimates by overcoming the issues apparent in the use of the classical d18O slope method. It can at the same time resolve temperature signals at low and high frequencies.
description: The overlapping NGRIP I and II core sampled with a 5 cm resolution an measured on an IRMS. Even though the depth is identical, it is not expected that the age is completely identical.
description: Supplement to: Gkinis, Vasileios; Simonsen, Sebastian B; Buchardt, Susanne L; White, James W C; Vinther, Bo Møllesøe (2014): Water isotope diffusion rates from the NorthGRIP ice core for the last 16,000 years – Glaciological and paleoclimatic implications. Earth and Planetary Science Letters, 405, 132-141