cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.974360
title: Secondary standards for major oxide concentrations of individual glass tephra shards from the Greenland ice core TUNU2013_58.04-58.14m, Summit2023_180.52-108.69m, and Summit2023_108.22-108.37m samples

description: Secondary standards of Lipari, BCR-2Ga, ML3B-G, StHS6/80-G, and Old Crow for major element oxide tephra glass analyses obtained from individual glass shards from samples TUNU2013_58.04-58.14m, Summit2023_180.52-108.69m, and Summit2023_108.22-108.37m in the Greenland TUNU2013 [78.04°N/33.88°W] and Summit2023 [72.6°N/38.3°W] ice cores. Normalised analytical data (totals to 100%) and the original analytical totals are reported (before normalisation) all as weight %. Data was obtained using electron probe micro-analysis (EPMA) at the University of Bern, Switzerland and the University of St Andrews, UK.
DOI: 10.13130/rd_unimi/n9enq4/izm8tx
title: opt-186.txt

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/wsbtse
title: edges_init-166.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/cpo1oe
title: edge_data_final-183.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.979555
title: Highly branched isoprenoids in lake sediments

description: Diatom-derived highly branched isoprenoids (HBIs) are found extensively in marine sediments, but are observed in a limited number of lake sediments. To expand on this record, between 2022 and 2024, we collected lake surface sediment samples from 50 lakes in the United States of America from the Midwest and Northeast. Studied lakes capture a range in climate, water chemistry (e.g., pH, salinity, alkalinity), size, and trophic states. Lakes also vary in their diatom species compositions. Surface sediment samples were collected using a gravity corer or a Bolivia-type square-rod piston corer deployed from a boat. Lake sediments were extracted and analyzed for their HBI compounds and concentrations by gas chromatography mass spectrometry. Lake surface sediments were analyzed for their carbon and nitrogen concentrations and stable isotopes.
DOI: 10.13130/rd_unimi/n9enq4/ea2toc
title: edge_data_final-196.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.977780
title: May-June 2023 California Current Thermosalinograph Data

description: Oceanographic properties were measured during the Phytoplankton UPwelling response CYCLE (PUPCYCLE) II expedition May 27-June 12, 2023 during a transit between Newport, OR and San Francisco, CA onboard the R/V Sally Ride. Temperature and salinity were measured with a SBE 45 MicroTSG connected to ship's seawater supply line (~5m nominal depth). Chlorophyll and Oxygen concentrations were measured with a Seabird Chlorophyll Fluorometer and an oxygen optode, respectively.
DOI: 10.13130/rd_unimi/n9enq4/ft0l5m
title: opt-179.txt

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/hv8boa
title: opt-185.txt

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/tkoeg9
title: edge_data_final-175.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/6ldkql
title: nodes_init-181.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/f1c11x
title: force_disp_final-179.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.928408
title: Element analysis of sediment core JR298-PC726
DOI: 10.13130/rd_unimi/n9enq4/eec8rn
title: edges_final-161.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/dktwjm
title: force_disp_final-189.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/pxvqtp
title: force_disp_init-161.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/mcl4eg
title: edges_final-191.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/9oxzsa
title: force_disp_init-166.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.974359
title: Major oxide concentrations of individual glass tephra shards from the Greenland ice core TUNU2013_58.04-58.14m, Summit2023_180.52-108.69m, and Summit2023_108.22-108.37m samples

description: Major oxide concentrations of individual glass tephra shards from tephra deposits in the Greenland TUNU2013 [78.04°N/33.88°W] and Summit2023 [72.6°N/38.3°W] ice cores. Deposits analysed are (i) TUNU2013_58.04-58.14m, (ii) Summit2023_180.52-108.69m, and (iii) Summit2023_108.22-108.37m. Normalised analytical data (totals to 100%) and the original analytical totals are reported (before normalisation) all as weight %. Data was obtained using electron probe micro-analysis (EPMA) at the University of Bern, Switzerland and the University of St Andrews, UK. Sample ID, sample depth (m), sample age (Year CE), tephra name (if known), source volcano, and normalised oxide values are provided.
DOI: 10.13130/rd_unimi/n9enq4/6tgp3k
title: nodes_final-155.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/yeufnd
title: force_disp_init-191.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.928511
title: Magnetic susceptibility of sediment core JR298-GBC722
DOI: 10.1594/pangaea.942935
title: Surface meteorological and ceilometer measurements near the Salton Sea on 2020-02-22
DOI: 10.13130/rd_unimi/n9enq4/vgyfms
title: edge_data_final-170.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.928470
title: Element analysis of sediment core PS1565-2
DOI: 10.1594/pangaea.943344
title: Diatom abundance of sediment core KNR197-10CDH42
DOI: 10.13130/rd_unimi/n9enq4/ije0h7
title: nodes_init-170.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/lxqx4v
title: edges_final-175.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.928467
title: Discrete element analysis of sediment core JR298-PC727
DOI: 10.13130/rd_unimi/n9enq4/zksnbp
title: nodes_final-180.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.946792
title: Age-Depth tie points for drill core ANDRILL 2A

description: Age tie points from 214.13 mbsf and above from: Acton et al. (2008). Age tie points from 214.14 to 1138.54 mbsf from Levy et al. (2016).Antarctica New Zealand Sir Robin Irvine PhD Scholarship awarded to B.D. Scientific Committee of Antarctic Research Fellowship awarded to B.D. New Zealand Ministry of Business Innovation and Employment through the Antarctic Science Platform (ANTA1801), and Contract C05X1001
DOI: 10.1594/pangaea.946797
title: Age-Depth tie points for DSDP Hole 28-274

description: Ages have been assigned using the relaxed hybrid CONOP model of Crampton et al. (2016). No biostratigraphic markers exist in the interval directly below 141.26 so the age model here assumes the same sedimentation rate as between 113.6 and 141.26.Age tie points from 214.13 mbsf and above from: Acton et al. (2008). Age tie points from 214.14 to 1138.54 mbsf from Levy et al. (2016).Antarctica New Zealand Sir Robin Irvine PhD Scholarship awarded to B.D. Scientific Committee of Antarctic Research Fellowship awarded to B.D. New Zealand Ministry of Business Innovation and Employment through the Antarctic Science Platform (ANTA1801), and Contract C05X1001
DOI: 10.13130/rd_unimi/n9enq4/qr3uqe
title: force_disp_init-164.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/x1jgcs
title: nodes_init-167.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.960033
title: Environmental CTD data at time series station BATS from March-2016 till May-2017

description: Data were obtained as part of the Bermuda Atlantic Time-series Study (BATS) in order to characterise the environmental context of the ecosystem. They were collected on board of the R/V Atlantic Explorer, at BATS site (31°40′N; 64°10′W) on a monthly basis, from March 2016 to May 2017, except in March 2017 due to rough weather. Environmental samples were taken during the day, except in February 2017 when they were taken at night. Environmental data were collected vertically using a SeaBird 911 CTD rosette equipped with temperature (°C), conductivity (mS/cm), fluorescence (RFU), oxygen (µmol/kg) and Photosynthetic Active Radiation (PAR, µE/m²s) sensors. Density (σθ) was calculated from temperature and conductivity. Depth of the Deep Chlorophyll Maximum (DCM, m) was defined as the maximum of the fluorescence profile. Three types of Mixed Layer Depth (MLD, m) were calculated. A seasonal and a depth zone characterisation were obtained from MLD, DCM and density measures. The depth (m) at which the light intensity was equal to 1% of the surface light intensity was also computed.
DOI: 10.1594/pangaea.967365
title: Benthic foraminifera stable carbon isotopes of ODP Site 145-883

description: Here we present same sample measurements of C. wuellerstorfi and U. proboscidea stable carbon isotopes from ODP sites 883 and 887. Samples were freeze dried, weighed, soaked in water for 24 hours to disaggregate, and wet sieved using a 150 μm mesh sieve. Samples were then dried at 40°C. Select genera and species were picked and comprehensively counted from the 150–355 μm fraction. Cibicidoides wuellerstorfi and Uvigerina probuscidea were both measured in 84 samples. Specimens selected for isotopic analysis were cleaned with 70 μL ethanol and sonicated for 30 seconds. Ethanol was drawn off with a pipette, and specimens were dried overnight at room temperature. Isotope ratios were quantified at the Brown University stable isotope facility with a Finnigan Mat 252 with Carbonate Kiel III autosampler, in which individual samples were reacted with 70°C H3PO4.
DOI: 10.13130/rd_unimi/n9enq4/slomfh
title: opt-154.txt

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.967367
title: GRAPE density of ODP Site 145-883

description: New composite GRAPE WBD profile from our new splice at ODP site 883. The composite depth scale was created by visual correlation of the shipboard gamma ray attenuation and porosity evaluator (GRAPE) wet bulk density (WBD) measurements between 883B and 883C starting at core 10H and ending at 18H. 883B 11H-1 0–57 cm, 883B 12H-1 0–10 cm, 883B 15H-1 0–20 cm, 883C 15H-1 0–5 cm were not considered in the correlation exercise because the recovered sediments had sidewall cave-in characterized by pebbles typical of the overlying Pleistocene sediments. In almost all cores, recovery was &gt; 100%. To account for this in terms of depth, cores with &gt; 100% recovery were compressed uniformly and fixed to the top drill log depth (depth mbsf) assigned to that core. Subsequent correlation of cores between holes B and C revealed apparent gaps in recovery. Cores were further uniformly compressed to account for the unrecovered sediments and a composite stratigraphic section was stitched together by switching between the two holes. On average, cores were compressed 17% and at most by 28% of their drilled depth (9.5 m). The result of this exercise is a composite section of comparable depth to the driller's shipboard depth scale (109.4 meters below sea floor vs. 108.3 meters common depth) that accounts for all the major stratigraphic features present in the GRAPE WBD profiles of 883B and 883C.
DOI: 10.1594/pangaea.967376
title: GRAPE density of ODP Site 145-887

description: New composite GRAPE WBD profile from our new splice at ODP site 887. The composite depth scale for site 887 was created by visual correlation of the shipboard GRAPE WBD measurements between 887A and 887C cores 11H and 12H. 887C 11H-1 0–12 cm and 887C 12H-1 0-35 were not considered in the correlation exercise due to flow in and heavy core disturbance noted by the shipboard scientific party. In almost all cores, recovery was &gt; 100%. To account for this in terms of depth, cores with &gt; 100% recovery were compressed uniformly and fixed to the top drill log depth (depth mbsf) assigned to that core. Subsequent correlation of cores between holes A and C revealed apparent gaps in recovery. Cores were further uniformly compressed to account for the unrecovered sediments and a composite stratigraphic section was stitched together by switching between the two holes. On average, cores were compressed 10% and at most by 25% of their drilled depth (9.5 m). GRAPE WBD from 887A and 887C was then correlated to the composite section to generate tie points for each core to the composite section.
DOI: 10.13130/rd_unimi/n9enq4/b1pqwn
title: nodes_final-150.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/e943fq
title: force_disp_init-158.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.971080
title: Major and trace elements in surface inputs to Deming Lake, MN, USA (2022-2023)

description: Several sites around Itasca State Park that are potentially representative of input sources to Deming Lake were sampled in August 2023. Water from a bog on the southeast margin of Deming Lake represent surface inputs, and water from springs along Nicollet Creek, and from Elk Spring on the margins of Elk Lake represent regional groundwaters. These were sampled with syringes fit 0.22 μm syringe filters, waters were acidified at the University of Minnesota Itasca Biological Station. Water elemental compositions were determined using a Thermo Fisher iCAP-Q inductively coupled plasma mass spectrometer (ICP-MS) at the WHOI Plasma Facility following 200 dilution of a 10 μL aliquot in 2 % HNO3. Indium (In) was added to samples at a concentration of 1 ng/g prior to analyses to monitor and correct for instrument drift by normalizing to In intensities. Concentrations were calculated using a five-point calibration curve obtained by fitting of ion beam intensities measured for serial dilutions of a gravimetrically prepared multi-element standard. The relative standard deviation (RSD) for five measurements of each sample was ~10% on the iCAP-Q. The accuracy and precision of similar concentration measurements on iCAP-Q at WHOI have previously been determined to be ± 5-10 % (1SD) based on comparison with USGS reference materials AGV-1, AGV-2, BHVO-1, BHVO-2, BIR-1, and BCR-2 prepared and analyzed as unknowns during earlier runs (Jochum et al., 2016; Shu et al., 2017).
DOI: 10.13130/rd_unimi/n9enq4/rphcah
title: opt-150.txt

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.935510
title: Oxygen isotope analyses (d18O) by gas source mass spectrometry in pooled N. pachyderma shells from plankton tows deployed in the Fram Strait
DOI: 10.1594/pangaea.966670
title: Bulk grain size of sediment core MVSEIS08_TG-2 from Gulf of Cadiz

description: 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 min. Prior to grain-size analysis in a Sedigraph Micromeritics III Plus, samples were homogenised by stirring in a magnetic plate for 30 min.
DOI: 10.13130/rd_unimi/n9enq4/fdszae
title: edges_init-161.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/wg5wln
title: edges_init-162.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.966663
title: Stable isotopes of planktonic and benthic foraminifera of sediment core MVSEIS08_TG-2 from Gulf of Cadiz

description: For stable O and C isotopes analysis, 25 planktonic and 10 benthic foraminifera of the species Globigerina bulloides and Cibicides pachyderma were picked primarily in the fraction &gt;250 μm, and occasionally in the interval 150–250 μm, in 113 samples, at the IGME. The analyses were performed in a Finnigan MAT 252 mass spectrometer at Marum (University Bremen, Germany), coupled to an automated Kiel-carbonate preparation system. The long-term precision is ±0.07‰ for δ18O and ±0.05‰ for δ13C based on repeated analyses of internal and external (NBS-19) carbonate standards. The stable O and C ratios are expressed as δ in permil (‰), relative to Vienna Peedee Belemnite (VPDB) standard. Nine duplicated samples in TG2 give a standard deviation between 0.07 and 0.12‰.
DOI: 10.1594/pangaea.966665
title: Stable isotopes of planktonic and benthic foraminifera of sediment cores GC-01A from Gulf of Cadiz

description: For stable O and C isotopes analysis, 25 planktonic and 10 benthic foraminifera of the species Globigerina bulloides and Cibicides pachyderma were picked primarily in the fraction &gt;250 μm, and occasionally in the interval 150–250 μm, in 113 samples, at the IGME. The analyses were performed in a Finnigan MAT 252 mass spectrometer at Marum (University Bremen, Germany), coupled to an automated Kiel-carbonate preparation system. The long-term precision is ±0.07‰ for δ18O and ±0.05‰ for δ13C based on repeated analyses of internal and external (NBS-19) carbonate standards. The stable O and C ratios are expressed as δ in permil (‰), relative to Vienna Peedee Belemnite (VPDB) standard. Nine duplicated samples in TG2 give a standard deviation between 0.07 and 0.12‰.
DOI: 10.13130/rd_unimi/n9enq4/lubxwq
title: nodes_init-179.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.956147
title: PlioVAR sea surface temperature (SST) anomaly calculation
DOI: 10.1594/pangaea.966841
title: Climate associations of planktic foraminifera of sediment cores GC-01A 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: 10.13130/rd_unimi/n9enq4/1h0c9j
title: force_disp_init-193.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.956144
title: Compiled Uk'37 data from PlioVAR
DOI: 10.13130/rd_unimi/n9enq4/8yrn01
title: nodes_final-187.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.13130/rd_unimi/n9enq4/kjryfv
title: opt-190.txt

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.1594/pangaea.913797
title: Shallow seismicity and the classification of structures in the Lau back-arc basin

description: We compared Centroid Moment Tensors (CMTs), calculated for large (Mw &gt;5), shallow (&lt;30 km) seismic events to the orientations of seafloor lineaments (n = 4000) mapped throughout the Lau Basin, in the SW Pacific. Ship-based multibeam was combined with vertical gravity gradient data to provide comprehensive coverage to create the lineament map. By comparing the possible focal planes of the CMTs to the orientations of the lineaments, the most likely fault plane solutions were selected, thus classifying the faults and establishing the nature of the highly variable stress regimes in the basin. We resolved the strike, dip and dip direction of 308 faults, and classified 258 additional structures by fault type. The majority of the table was data downloaded from the Global Centroid Moment Tensor (GCMT) database (www.globalcmt.org: accessed October 2018). For more details about the column headers consult the GCMT database website. New data from this study include the latitude and longitude error estimates (in meters), the classified faults (column: 'fault_type'), and the stress domain (column: 'stress_domain'), allocated to each of the classified faults.
DOI: 10.13130/rd_unimi/n9enq4/rjhmlh
title: nodes_final-177.dat

description: 250729_SIMULATION_DATA/TENS-N_1.zip
DOI: 10.3535/abj-dz2-ldk
title: Bison C. H. Smith, 1827

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/rs1-h1h-7nt
title: Isurus

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/hzp-ne3-39v
title: Phacops

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/wpm-s6g-bz1
title: Mammalia Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/7zm-sl7-x8w
title: Animalia

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/1s4-1z5-k9b
title: Megabalanus

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/epw-24h-bsg
title: Mammalia Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.17632/6yxrmwz3n3
title: Insights into the evolution of pore structure and novel stress sensitivity determination of porosity-permeability in unconventional rocks

description: Data
DOI: 10.3535/7fr-779-bl1
title: Cnidaria

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/ejw-051-25t
title: Mammalia Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/2bf-x34-5l6
title: †Anticostiella Copeland, 1973

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/96j-xmf-dvv
title: Mammalia Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.17632/6yxrmwz3n3.1
title: Insights into the evolution of pore structure and novel stress sensitivity determination of porosity-permeability in unconventional rocks

description: Data
DOI: 10.3535/mld-sdz-txm
title: Odontaspis

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/k8l-y82-hvb
title: Balclutha Kirkaldy, 1900

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/qa6-1z4-cvq
title: Equus (Equus) caballus Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/6wr-152-lqh
title: Mammalia Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.
DOI: 10.3535/jnt-ldp-czz
title: Mammalia Linnaeus, 1758

description: Digital Specimen for the physical specimen hosted at Naturalis Biodiversity Center.