cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.966213
title: Dissolved nutrients data from the PS122 MOSAiC Expedition carried out onboard Polarstern during Legs 1 to 3

description: Samples for the analysis of dissolved nutrients were collected during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) from the water column, sea ice cores and from special events/locations (e.g., leads, melt ponds, brine, incubation experiments). Samples for dissolved inorganic nutrients (NO3 +NO2 , NO2 , PO4 , Si(OH)4, NH4 ) were analysed onboard during PS122 legs 1 to 3, with duplicate samples collected from CTD casts for later analysis of total dissolved nitrogen (TDN) and total dissolved phosphorus (TDP). From leg 4, all samples collected were stored frozen at -20°C for later analysis. Analyses of stored samples were carried out at the AWI Nutrient Facility between January and March 2021. Nutrient analyses onboard and on land were carried out using a Seal Analytical AA3 continuous flow autoanalyser, controlled by the AACE software version 7.09. Best practice procedures for the measurement of nutrients were adopted following GO-SHIP recommendations (Hydes et al., 2010; Becker et al., 2019). Descriptions of sample collection and handling can be found in the various cruise reports (Haas & Rabe, 2023; Kanzow & Damm, 2023; Rex & Metfies, 2023; Rex & Nicolaus, 2023; Rex & Shupe, 2023). Here we provide data from the water column, obtained from the analysis of discrete samples collected from CTD-Rosette casts from Polarstern (https://sensor.awi.de/?site=search&q=vessel:polarstern:ctd_sbe9plus_321) and Ocean City (https://sensor.awi.de/?site=search&q=vessel:polarstern:ctd_sbe9plus_935). Data from sea ice cores and special events are presented elsewhere. Data from sea ice cores and special events are presented elsewhere. For reference, here we included data from CTD-BTL files associated with nutrient samples. These data are presented by Tippenhauer et al. (2023) Polarstern CTD and Tippenhauer et al. (2023) Ocean City CTD.
DOI: 10.13130/rd_unimi/n9enq4/zpzaej
title: opt-129.txt

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.943341
title: Stable carbon isotopes measured on foraminifer Uvigerina peregrina of sediment core KNR197-10CDH42
DOI: 10.1594/pangaea.966614
title: Age model of sediment cores GC-01A from Gulf of Cadiz

description: For AMS 14C ages, approximately 10 mg of planktonic foraminifera species (Globigerina bulloides, Globigerinoides ruber-white, Globorotalia inflata, Globigerina falconensis, Globorotalia truncatulinoides and Orbulina universa) were picked in the fraction &gt;150 or &gt;250 μm. AMS radiocarbon ages were calibrated using the Calib program (Stuiver and Reimer, 1993) on-line version 6.0 (http://calib.qub.ac.uk) and the Marine09 calibration data (Reimer et al., 2009). Between 0 and 10.5 cal ka BP the Marine09 dataset is based on the Intcal09 tree-ring data that was converted with an ocean - atmosphere box diffusion model to yield ocean mixed-layer ages (Hughen et al., 2004). Beyond 10.5 kyr it uses marine coral and varve data with a mean global reservoir correction of 405 years (Reimer et al., 2009).
DOI: 10.13130/rd_unimi/n9enq4/azurws
title: force_disp_final-142.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.13130/rd_unimi/n9enq4/wckfup
title: edges_final-145.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.966839
title: Sortable silt of sediment cores GC-01A from Gulf of Cadiz

description: For sortable-silt 83 samples were analysed in the fraction &lt;63 micron. In these, organic matter was eliminated with 33% of hydrogen peroxide (H2O2) and carbonates removed with 0.2N hydrogen chloride (HCl). Then, samples were dispersed with 0.5% Na-hexametaphosphate (Calgon) and ultra-sonicated for 2 minutes. Prior to grain-size analysis in a Sedigraph Micromeritics III Plus, samples were homogenised by stirring in a magnetic plate for 30 minutes. The grain-size distribution was acquired in the interval 10-63 micron, assumed to have non-cohesive behaviour during transport and deposition (McCave et al., 1995), at the IGME. The sortable silt mean of the carbonate-free 10-63 micron interval is designated as SS (McCave et al., 1995). The percentage of sortable silt (SS%), i.e. % (10-63 micron)/&lt;63 micron, is also a key parameter obtained from Sedigraph analyses. Dry-density required for the grain size distribution calculation was measured by using a pycnometer Micromeritics Accupy 1330.
DOI: 10.13130/rd_unimi/n9enq4/ixyc16
title: nodes_init-111.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.966613
title: Age model of sediment core MVSEIS08_TG-2 from Gulf of Cadiz

description: For AMS 14C ages, approximately 10 mg of planktonic foraminifera species (Globigerina bulloides, Globigerinoides ruber-white, Globorotalia inflata, Globigerina falconensis, Globorotalia truncatulinoides and Orbulina universa) were picked in the fraction &gt;150 or &gt;250 μm. AMS radiocarbon ages were calibrated using the Calib program (Stuiver and Reimer, 1993) on-line version 6.0 (http://calib.qub.ac.uk) and the Marine09 calibration data (Reimer et al., 2009). Between 0 and 10.5 cal ka BP the Marine09 dataset is based on the Intcal09 tree-ring data that was converted with an ocean - atmosphere box diffusion model to yield ocean mixed-layer ages (Hughen et al., 2004). Beyond 10.5 kyr it uses marine coral and varve data with a mean global reservoir correction of 405 years (Reimer et al., 2009).
DOI: 10.1594/pangaea.966842
title: Element ratios from XRF-scan of sediment core MVSEIS08_TG-2 from Gulf of Cadiz

description: The content of a series of elements, included Zr (30 kV) and Ca, Al, Si, Fe (10 kV), were measured by non-destructive, continuous X-ray fluorescence (XRF) in cts (counts per second per unit area) every 1 cm, using an Avaatech core scanner at the University of Barcelona.
DOI: 10.13130/rd_unimi/n9enq4/ptg8i6
title: edge_data_final-139.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.13130/rd_unimi/n9enq4/riubvy
title: force_disp_init-133.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.966840
title: Climate associations of planktic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz

description: For planktonic foraminifera counts, 9–12 cc of 68 bulk sub-samples were wet-weighed, freeze-dried, and re-weighed, then ultra-sonicated in a water bath, washed and sieved with tap and distilled water at the end through two grain-size fractions (63–150 μm and &gt;150 μm) at the IGME. These fractions were dried on paper filters in the oven at 40 °C and weighed. Samples in the fraction &gt;150 μm were split into adequate aliquots of at least 300–400 individuals for planktonic foraminifera census. The identification of species follows the taxonomy of Loeblich and Tappan (1964). Biogenic groups other than foraminifera and detrital minerals were counted in the same sample split. To trace the temperature of the surface water masses, planktonic foraminifera species were counted and classified into four assemblages, following the studies in the area (Bé and Tolderlund, 1971; Hemleben et al., 1989; Kucera, 2007; Reguera, 2001, 2004): polar (Neogloboquadrina pachyderma), subpolar (Neogloboquadrina incompta, Neogloboquadrina pachyderma-dutertrei, Neogloboquadrina dutertrei, Globigerina bulloides, Turborotalita quinqueloba), transitional (Globorotalia uvula, Globorotalia scitula, Globorotalia glutinata, Globorotalia inflata, Orbulina universa, Globorotalia truncatulinoides, Globorotalia hirsuta) and subtropical (Globigerinoides ruber-white, Globigerinoides ruber-pink, Globorotalia crassaformis, Globorotalia aequilateralis, Globigerina rubescens, Globigerina falconensis, Globigerinoides trilobus, Globigerinoides sacculifer).
DOI: 10.1594/pangaea.967070
title: Physical properties of sediment cores GC-01A from Gulf of Cadiz

description: Sediment physical properties as wet density (gamma-ray) in g/cc and P-wave velocity in m/s, were quantified on the three cores using a Geotech Multi-sensor Core Logger (MSCL) at the IGME, of continuous non-destructive acquisition in depth interval of 1 cm" (Suppl.Materials of Lebreiro et al. QSR, 2018).
DOI: 10.13130/rd_unimi/n9enq4/fu7z4i
title: edges_init-124.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.967179
title: Reflectance of sediment cores GC-01A from Gulf of Cadiz

description: Optical properties of sediment give 2 RGB colour combinations (L*a*b* system for sediment color analyses) which characterize particular features of the mineralogical and geochemical composition of the sediment. The CIE (Commission Internationale d'Eclairage) L* lightness parameter, partly correlated with CaCO3, organic carbon and oxides content, was measured with a Linescan V1.8 of Avaatech, in the visible spectrum, lens aperture of 8 mm, 5 msec time of exposure, and space resolution of 0.07m, at the University of Barcelona, Spain.
DOI: 10.1594/pangaea.968040
title: Sea surface temperatures derived from sediment core MVSEIS08_TG-2 from Gulf of Cadiz

description: Counts of planktonic foraminifera (&gt;150 μm) were converted into Sea Surface Temperatures (SST) through a transfer function based on modern analogues; we applied SIMMAX28 (Modern Analogue Technique using a similarity index).
DOI: 10.13130/rd_unimi/n9enq4/5e5kf0
title: nodes_final-125.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.13130/rd_unimi/n9enq4/m9ejlx
title: edges_init-107.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.967069
title: Physical properties of sediment core MVSEIS08_TG-2 from Gulf of Cadiz

description: Sediment physical properties as wet density (gamma-ray) in g/cc and P-wave velocity in m/s, were quantified on the three cores using a Geotech Multi-sensor Core Logger (MSCL) at the IGME, of continuous non-destructive acquisition in depth interval of 1 cm" (Suppl.Materials of Lebreiro et al. QSR, 2018).
DOI: 10.1594/pangaea.968042
title: Sea surface temperatures derived from sediment cores GC-01A from Gulf of Cadiz

description: Counts of planktonic foraminifera (&gt;150 μm) were converted into Sea Surface Temperatures (SST) through a transfer function based on modern analogues; we applied SIMMAX28 (Modern Analogue Technique using a similarity index).
DOI: 10.13130/rd_unimi/n9enq4/iijbxd
title: edge_data_final-105.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.967180
title: Reflectance of sediment core MVSEIS08_TG-2 from Gulf of Cadiz

description: Optical properties of sediment give 2 RGB colour combinations (L*a*b* system for sediment color analyses) which characterize particular features of the mineralogical and geochemical composition of the sediment. The CIE (Commission Internationale d'Eclairage) L* lightness parameter, partly correlated with CaCO3, organic carbon and oxides content, was measured with a Linescan V1.8 of Avaatech, in the visible spectrum, lens aperture of 8 mm, 5 msec time of exposure, and space resolution of 0.07m, at the University of Barcelona, Spain.
DOI: 10.13130/rd_unimi/n9enq4/rnojmn
title: force_disp_init-142.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.931020
title: SST reconstruction for sediment core MD11-3353
DOI: 10.1594/pangaea.931024
title: Diatom bound nitrogen isotopes of sediment core MD12-3394
DOI: 10.13130/rd_unimi/n9enq4/m3wb27
title: nodes_final-140.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.13130/rd_unimi/n9enq4/ypcckf
title: nodes_final-127.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.931017
title: Chronology of sediment core MD11-3353
DOI: 10.13130/rd_unimi/n9enq4/j7nfeo
title: nodes_final-101.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.931030
title: Mean nitrogen isotopes of sediment cores MD12-3394 and MD11-3353
DOI: 10.1594/pangaea.972377
title: Leaf wax δ2Hprecip and δ13C in sediments of tropical African alpine lake Africa over the Holocene

description: Lake sediment cores were collected from the Rwenzori Mountains, Uganda-Democratic Republic of Congo from three lakes: Lake Kopello (4,017 m asl), Lake Africa (3,895 m asl), and Lake Mahoma (2,990 m asl). Analysis of the recovered cores focused on the late Pleistocene and Holocene at centennial resolution. Sediments were prepared for biomarker analysis, and we report leaf wax δ2Hprecip and δ13Cwax. These data provide the montane climate and vegetation history of the Rwenzori Mountains at varying elevations.
DOI: 10.1594/pangaea.972378
title: Leaf wax δ2Hprecip and δ13C in sediments of tropical African alpine lake Kopello over the Holocene

description: Lake sediment cores were collected from the Rwenzori Mountains, Uganda-Democratic Republic of Congo from three lakes: Lake Kopello (4,017 m asl), Lake Africa (3,895 m asl), and Lake Mahoma (2,990 m asl). Analysis of the recovered cores focused on the late Pleistocene and Holocene at centennial resolution. Sediments were prepared for biomarker analysis, and we report leaf wax δ2Hprecip and δ13Cwax. These data provide the montane climate and vegetation history of the Rwenzori Mountains at varying elevations.
DOI: 10.13130/rd_unimi/n9enq4/efh7sq
title: edge_data_final-127.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.13130/rd_unimi/n9enq4/q0mywi
title: edge_data_final-106.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.972379
title: Leaf wax δ2Hprecip and δ13C in sediments of tropical African alpine lake Mahoma over the Holocene

description: Lake sediment cores were collected from the Rwenzori Mountains, Uganda-Democratic Republic of Congo from three lakes: Lake Kopello (4,017 m asl), Lake Africa (3,895 m asl), and Lake Mahoma (2,990 m asl). Analysis of the recovered cores focused on the late Pleistocene and Holocene at centennial resolution. Sediments were prepared for biomarker analysis, and we report leaf wax δ2Hprecip and δ13Cwax. These data provide the montane climate and vegetation history of the Rwenzori Mountains at varying elevations.
DOI: 10.13130/rd_unimi/n9enq4/lfxrn9
title: opt-104.txt

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.932873
title: Cation concentrations within soil porewaters from the Cole Farm watershed
DOI: 10.1594/pangaea.966843
title: Element ratios from XRF-scan of sediment cores GC-01A from Gulf of Cadiz

description: The content of a series of elements, included Zr (30 kV) and Ca, Al, Si, Fe (10 kV), were measured by non-destructive, continuous X-ray fluorescence (XRF) in cts (counts per second per unit area) every 1 cm, using an Avaatech core scanner at the University of Barcelona.
DOI: 10.13130/rd_unimi/n9enq4/abcsb8
title: force_disp_final-133.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.13130/rd_unimi/n9enq4/x10g84
title: edges_final-104.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.934420
title: Intercalibrated dataset of in situ dissolved organic matter fluorescence from ice tethered profile 93 in the Central Arctic (2015-2016)

description: Here we present a merged and calibrated dataset of temperature, practical salinity and dissolved organic matter (DOM) fluorescence obtained from several Ice Tethered Profilers (ITPs) deployed across the central Arctic (2011-2016). The data offer a unique spatial coverage of the distribution of DOM in the surface 800 m below Arctic sea ice. A total of 5044 profiles are gathered. The ITP data are level 3 data products pressure-bin-averaged at 1-db vertical resolution with depth down to either 200 or approximately 750 m. Data (max 800m depth) from CTD casts made during two oceanographic cruises are also included. These were used as part of the calibration and validation of the ITP calibration routines. The cruises were PS94 (ARK-XXIX/3) with POLARSTERN in 2015 and NAACOS with DANA in 2012. The presented DOM fluorescence data are smoothed, corrected for instrument drift and calibrated to provide intercomparable data across the sensors. Fluorescence is reported in Raman Units (nm-1), and comparable to laboratory measurements conducted according to current community recommendations.
DOI: 10.13130/rd_unimi/n9enq4/scma3q
title: edge_data_final-114.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.854349
title: Annotated record of the detailed examination of Mn deposits from OSIRIS cruise stations

description: The cores and dredges described at this site were taken on the OSIRIS I cruise from 29 april until 7 june 1973 by the Muséum National d'Histoire Naturelle from the R/V Marion Dufresne. A total of 54 cores and dredges were recovered and are available at MNHN for sampling and study.
description: From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
description: Supplement to: MNHN (1973): OSIRIS I Cruise - MD00, R/V Marion Dufresne, Core list. Muséum National d'Histoire Naturelle, Paris, unpublished
DOI: 10.13130/rd_unimi/n9enq4/v3nybl
title: nodes_init-122.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.13130/rd_unimi/n9enq4/vuwkeb
title: nodes_final-102.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.932872
title: Anion concentrations within soil porewaters from the Cole Farm watershed
DOI: 10.1594/pangaea.972508
title: Continuous Antarctic Carbon monoxide (CO) record from Jurassic ice core from 1820 to 1995 CE

description: Continuous ice core carbon monoxide (CO) mixing ratios are presented for three West Antarctic Cores (Jurassic, Bryan Coast, and Dyer Plateau). Data cover from 1820 CE to 1995 CE. For each core, data are presented integrated at 10-second intervals from an original acquisition rate of 4 Hz. Data were measured continuously utilising Optical Feedback Cavity Enhanced Spectroscopy connected to a continuous ice core melting system at the British Antarctic Survey. A smoothed spline composed of the bottom 5th percentile of each record is also presented. A percentile re-sampling method is required to remove the impact of in situ production. The spline is used to interpret Southern Hemisphere CO variability from the pre-industrial with a particular focus on biomass burning.
DOI: 10.13130/rd_unimi/n9enq4/6swmh7
title: edges_init-114.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.932875
title: Soil pCO2 and soil pO2 from the Cole Farm watershed
DOI: 10.13130/rd_unimi/n9enq4/fh2swj
title: edges_final-140.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.972510
title: Continuous Antarctic Carbon monoxide (CO) record from Bryan Coast ice core from 1820 to 1995 CE

description: Continuous ice core carbon monoxide (CO) mixing ratios are presented for three West Antarctic Cores (Jurassic, Bryan Coast, and Dyer Plateau). Data cover from 1820 CE to 1995 CE. For each core, data are presented integrated at 10-second intervals from an original acquisition rate of 4 Hz. Data were measured continuously utilising Optical Feedback Cavity Enhanced Spectroscopy connected to a continuous ice core melting system at the British Antarctic Survey. A smoothed spline composed of the bottom 5th percentile of each record is also presented. A percentile re-sampling method is required to remove the impact of in situ production. The spline is used to interpret Southern Hemisphere CO variability from the pre-industrial with a particular focus on biomass burning.
DOI: 10.1594/pangaea.972514
title: Continuous Antarctic Carbon monoxide (CO) record from Dyer Plateau ice core from 1820 to 1995 CE

description: Continuous ice core carbon monoxide (CO) mixing ratios are presented for three West Antarctic Cores (Jurassic, Bryan Coast, and Dyer Plateau). Data cover from 1820 CE to 1995 CE. For each core, data are presented integrated at 10-second intervals from an original acquisition rate of 4 Hz. Data were measured continuously utilising Optical Feedback Cavity Enhanced Spectroscopy connected to a continuous ice core melting system at the British Antarctic Survey. A smoothed spline composed of the bottom 5th percentile of each record is also presented. A percentile re-sampling method is required to remove the impact of in situ production. The spline is used to interpret Southern Hemisphere CO variability from the pre-industrial with a particular focus on biomass burning.
DOI: 10.13130/rd_unimi/n9enq4/gu0uvy
title: nodes_init-119.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.13130/rd_unimi/n9enq4/s60lyp
title: force_disp_final-127.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.972515
title: Continuous Antarctic Carbon monoxide (CO) record (spline from 3 ice cores) from 1820 to 1995 CE

description: Continuous ice core carbon monoxide (CO) mixing ratios are presented for three West Antarctic Cores (Jurassic, Bryan Coast, and Dyer Plateau). Data cover from 1820 CE to 1995 CE. For each core, data are presented integrated at 10-second intervals from an original acquisition rate of 4 Hz. Data were measured continuously utilising Optical Feedback Cavity Enhanced Spectroscopy connected to a continuous ice core melting system at the British Antarctic Survey. A smoothed spline composed of the bottom 5th percentile of each record is also presented. A percentile re-sampling method is required to remove the impact of in situ production. The spline is used to interpret Southern Hemisphere CO variability from the pre-industrial with a particular focus on biomass burning.
DOI: 10.1594/pangaea.972783
title: Plio-Pleistocene alkenone sea surface temperature and productivity at eastern equatorial Pacific IODP Site 321-U1338

description: Alkenone biomarker unsaturation estimates (Uk'37) of sea surface temperature (SST) and alkenone concentration and mass accumulation rate (C37total) data are obtained for eastern equatorial Pacific (EEP) Integrated Ocean Drilling Program Site 321-U1338. Newly acquired alkenone biomarker data were generated at Brown University according to sample preparation and analytical methods described in Herbert et al. (2021). The SST and productivity data are sampled at 3-kyr resolution and span four time intervals in the Plio-Pleistocene: a Pliocene interval (3.0-3.6 Ma), a Plio-Pleistocene interval (2.4-2.8 Ma), a mid-Pleistocene interval (1.4-1.7 Ma), and a Late Pleistocene interval (350-650 ka). Gradients in SST and productivity between the two EEP sites can be tracked over the four time intervals listed above.
DOI: 10.13130/rd_unimi/n9enq4/w4xn3x
title: edges_init-132.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip
DOI: 10.1594/pangaea.972782
title: Plio-Pleistocene alkenone sea surface temperature and productivity at eastern equatorial Pacific ODP Site 138-849

description: Alkenone biomarker unsaturation estimates (Uk'37) of sea surface temperature (SST) and alkenone concentration and mass accumulation rate (C37total) data are obtained for eastern equatorial Pacific (EEP) Ocean Drilling Program Site 138-849. Newly acquired alkenone biomarker data were generated at Brown University according to sample preparation and analytical methods described in Herbert et al. (2021). The SST and productivity data are sampled at 3-kyr resolution and span four time intervals in the Plio-Pleistocene: a Pliocene interval (3.0-3.6 Ma), a Plio-Pleistocene interval (2.4-2.8 Ma), a mid-Pleistocene interval (1.4-1.7 Ma), and a Late Pleistocene interval (350-650 ka). Gradients in SST and productivity between the two EEP sites can be tracked over the four time intervals listed above.
DOI: 10.13130/rd_unimi/n9enq4/glp7po
title: force_disp_init-148.dat

description: 250729_SIMULATION_DATA/TENS-M_1.zip