cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15468/dl.uw7gmg
title: Occurrence Download

description: A dataset containing 17 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Continent is Africa",
 "Country is South Africa",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Nassella neesiana (Trin. & Rupr.) Barkworth"
 ]
}

 The dataset includes 17 records from 4 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0069989-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.52606
title: (Table 3) Stable isotope data and sea surface temperature from benthic foraminifera in sediment core MD88-770
DOI: 10.1594/pangaea.803855
title: (Table 3) Sulphur isotopic composition of pyrite concretions from ODP Hole 164-994C and Site 164-997
DOI: 10.1594/pangaea.872145
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 44 (Holes 389, 390, 390A, 392 and 392A)

description: The western part of the North Atlantic Ocean holds clues to some of the most intriguing questions in marine geology. But because the geologic problems are many and varied, the sites of Leg 44 were multipurpose in nature. In particular, some of the targets were : 1) the Blake Nose, a spur of the Blake Plateau, to determine the nature, age, and origin of reef-like structures recognized on seismic profiles and 2) the Blake Outer Ridge, a long low ridge of sediments that forms the eastern boundary of the Blake-Bahama Basin, where we hoped to study the stratigraphy and sample supposed clathrates.
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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: Benson, William E; Enos, Paul; Freeman, Tom; Gradstein, Felix M; Murdmaa, Ivar O; Pastouret, L; Schmidt, Ronald R; Sheridan, Robert E; Stuermer, D H; Weaver, Fred M; Worstell, Paula J (1978): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XLIV, 1005 pp
DOI: 10.1594/pangaea.689700
title: Radiosonde M49_R324 during METEOR cruise M49 on 1978-09-01 13:35h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.875922
title: Heterococcolithophores and holococcolithophores in the Mediterranean Sea during the MedSeA and Meteor M84/3 cruises (May 2013, April 2011)

description: For all the absolute coccolithophore abundances during the Meteor M84/3 cruise, see Oviedo et al. (2017) doi:10.1594/PANGAEA.875202.
DOI: 10.1594/pangaea.805653
title: Pigments measured on water bottle samples at time series station BATS in 1996
DOI: 10.1594/pangaea.476548
title: Hydrochemistry measured on water bottle samples at station NAtl_1983_6N_37W/63

description: This data sets is part of a compilation by James Swift for the Java OceanAtlas software. Data are from various pre-WOCE sources, mainly with contributions and quality control from Joseph Reid (SIO) and NODC.
DOI: 10.1594/pangaea.857327
title: (Fig. 3b) Stable oxygen isotope ratios of planktonic foraminifera of sediment core EW9302-JPC8
DOI: 10.1594/pangaea.690036
title: Radiosonde M69_R044 during METEOR cruise M69 on 1984-08-13 22:21h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.846756
title: Stable oxygen isotopic composition of Neogloboquadrina pachyderma d of sediment core EW9302-JPC8
DOI: 10.1594/pangaea.689501
title: Radiosonde M49_R122 during METEOR cruise M49 on 1978-08-04 20:40h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.663738
title: Oceanography at CTD/bottle station IFREMER_0578
DOI: 10.1594/pangaea.689626
title: Radiosonde M49_R249 during METEOR cruise M49 on 1978-08-26 17:13h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.708051
title: (Table 2) Averages of microprobe analyses on Ni-rich magnesiowüstite and coexisting magnesioferrite spinel from DSDP Hole 91-596 sediments
DOI: 10.1594/pangaea.689257
title: Radiosonde M2_R297 during METEOR cruise M2 on 1965-11-19 10:25h

description: Height of tropause 16470 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.857332
title: (Fig. 3b) Stable oxygen isotope ratios of planktonic foraminifera of sediment core SU90-03
DOI: 10.1594/pangaea.698995
title: Pliocene-Pleistocene stable oxygen and carbon isotope ratios of Cibicidoides wuellerstorfi from ODP Site 162-981 in the North Atlantic

description: Depth is composite depth (mcd)
DOI: 10.1594/pangaea.883653
title: Annotated record of the detailed examination of Mn deposits off Newfoundland, North Atlantic

description: Measurements of Pb-210 activities, in conjunction with micropaleontological, geotechnical and sedimentological observations, on sediment cores have been used to characterize two distinctive bioturbation regimes on the continental slope and rise east of Newfoundland. On the rise (2600 m), excess Pb-210 is confined to the upper few centimeters of the coarser-grained sediments underlying the axis of the Western Boundary Undercurrent. The geological and geochemical evidence for a low rate of bioturbation in this high bottom current regime is consistent with a reduced population of deeper burrowing macrofauna, particularly the species Maldane sarsi. In contrast, a higher flux of organic-rich, fine-grained particulate material to the middle slope (1500 m water depth), and the comparatively stable sedimentological conditions that prevail in this low bottom current regime, have led to the active colonization of the sediment substrate by bioturbating organisms. Enhanced mixing of middle slope deposits is reflected by comparatively lower shear strengths within the upper 30 cm of the sediment column, and by the reduced variability of the sediment-depth distribution of the most abundant species of foraminifera. Excess Pb-210 has been transported downward from the sediment-water interface to depths greater than 12 cm. Some Pb-210 profiles from the middle slope can be interpreted in terms of a diffusion mixing model for which the biological mixing coefficients are of the order of 0.10-1.0 cm2/yr.Measurements of the two and three dimensional distribution of excess Pb-210 in one middle slope box core indicate that the mixing process in these sediments has a pronounced heterogeneous component on time scales of the same order as the half life of Pb-210 (22.3 yr). Spatial correlations between Pb-210 anomalies and artifacts of bioturbation observed in x-radiographs of the core suggest that Pb-210 maxima observed at depth may be the result of an inclined orientation of burrow structures which have introduced a significant lateral component to the downward transport of surficial sediments.
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: Smith, J N; Schafer, C T (1984): Bioturbation processes in continental slope and rise sediments delineated by Pb?210, microfossil and textural indicators. Journal of Marine Research, 42(4), 1117-1145
DOI: 10.1594/pangaea.896515
title: Images and morphometric features from Fragilariopsis kerguelensis valves

description: Valves of the diatom Fragilariopsis kerguelensis, sampled along four North-South transects across the Southern Ocean, were imaged in high resolution, extended depth-of focus light microscopic images. The images were segmented and morphometric features extracted using the software SHERPA.
description: Supplement to: Glemser, Barbara; Kloster, Michael; Esper, Oliver; Eggers, Sarah Lena; Kauer, Gerhard; Beszteri, Bánk (2019): Biogeographic differentiation between two morphotypes of the Southern Ocean diatom Fragilariopsis kerguelensis. Polar Biology, 42(7), 1369-1376
DOI: 10.1594/pangaea.665439
title: Oceanography at CTD/bottle station IFREMER_2279
DOI: 10.1594/pangaea.774728
title: (Table 1) Planktonic foraminifera counts and stable oxygen isotope ratios of Pacific Ocean surface sediments

description: Core-top samples from the eastern tropical Pacific (10°N to 20°S) were used to test whether the ratio between Globorotalia menardii cultrata and Neogloboquadrina dutertrei abundance (Rc/d) and the oxygen isotope composition (?18O) of planktonic foraminifera can be used as proxies for the latitudinal position of the Equatorial Front. Specifically, this study compares the ?18O values of eight species of planktonic foraminifera (Globigerinoides ruber sensu stricto (ss) and sensu lato (sl), Globigerinoides sacculifer, Globigerinoides triloba, Pulleniatina obliquiloculata, Neogloboquadrina dutertrei, Globorotalia menardii menardii, Globorotalia menardii cultrata and Globorotalia tumida) with the seasonal hydrography of the region, and evaluates the application of each species or combination of species for paleoceanographic reconstructions. The results are consistent with sea surface temperature and water column stratification patterns. We found that in samples north of 1°N, the Rc/d values tend to be higher and d18O values of G. ruber, G. sacculifer, G. triloba, P. obliquiloculata, N. dutertrei, and G. menardii cultrata tend to be lower than those from samples located south of 1°N. We suggest that the combined use of Rc/d and the d18O difference between G. ruber and G. tumida or between P. obliquiloculata and G. tumida are the most suitable tools for reconstructing changes in the latitudinal position of the Equatorial Front and changes in the thermal stratification of the upper water column in the eastern tropical Pacific.
description: Supplement to: Rincón-Martínez, Daniel; Steph, Silke; Lamy, Frank; Mix, Alan C; Tiedemann, Ralf (2011): Tracking the equatorial front in the eastern equatorial Pacific Ocean by the isotopic and faunal composition of planktonic foraminifera. Marine Micropaleontology, 79(1-2), 24-40
DOI: 10.1594/pangaea.689605
title: Radiosonde M49_R228 during METEOR cruise M49 on 1978-08-25 07:59h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.897491
title: (Table S19) Foraminiferal range charts of ODP Site 154-926 (5506-9678 ka)

description: P - indicates taxa present, ? - indicates questionable occurrence, - indicates absence.
DOI: 10.1594/pangaea.689499
title: Radiosonde M49_R120 during METEOR cruise M49 on 1978-08-04 18:27h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.6084/m9.figshare.24586105
title: Additional file 1 of LppA is a novel plasminogen receptor of Mycoplasma bovis that contributes to adhesion by binding the host extracellular matrix and Annexin A2

description: Additional file 1. Plasmids, oligonucleotides, cell lines and strains used in this study. List of plasmids, primers, M. bovis strains, and cell line used in this study.
DOI: 10.6084/m9.figshare.24586105.v1
title: Additional file 1 of LppA is a novel plasminogen receptor of Mycoplasma bovis that contributes to adhesion by binding the host extracellular matrix and Annexin A2

description: Additional file 1. Plasmids, oligonucleotides, cell lines and strains used in this study. List of plasmids, primers, M. bovis strains, and cell line used in this study.
DOI: 10.6084/m9.figshare.24586316
title: Additional file 2 of LppA is a novel plasminogen receptor of Mycoplasma bovis that contributes to adhesion by binding the host extracellular matrix and Annexin A2

description: Additional file 2. The strains information of MB-DATABASE and MY-DATABASE. NCBI accession numbers of strains used to construct the MB-DATABASE and MY-DATABASE databases. Genetic analysis of LppA sequences in Mycoplasmas and bacteria.
DOI: 10.6084/m9.figshare.24586316.v1
title: Additional file 2 of LppA is a novel plasminogen receptor of Mycoplasma bovis that contributes to adhesion by binding the host extracellular matrix and Annexin A2

description: Additional file 2. The strains information of MB-DATABASE and MY-DATABASE. NCBI accession numbers of strains used to construct the MB-DATABASE and MY-DATABASE databases. Genetic analysis of LppA sequences in Mycoplasmas and bacteria.
DOI: 10.1594/pangaea.633678
title: Physical oceanography measured on water bottle samples during POLARSTERN cruise ANT-XXIII/1

description: Sensors, processing and post-cruise calibration: interval = seconds: 0.0416667; sensor 0 = Frequency 0 temperature, primary, 2460, 21-oct-03; sensor 1 = Frequency 1 conductivity, primary, 2054, 31-oct-03, cpcor = -9.57; sensor 2 = Frequency 2 pressure, 68997, 07-21-1997; sensor 3 = Frequency 3 temperature, secondary, 2417, 16-jul-05; sensor 4 = Frequency 4 conductivity, secondary, 2055, 19-jul-05, cpcor = -9; sensor 5 = Extrnl Volt 0 userpoly 0, o2_SN:_48, 14-may-04; sensor 6 = Extrnl Volt 1 altimeter; sensor 7 = Extrnl Volt 2 transmissometer, primary, CST_267DR, 23-jul-99; sensor 8 = Extrnl Volt 4 userpoly 1, chl_6000meter, 1996; sensor 9 = Extrnl Volt 5 userpoly 2, ys_SN:8070_6000meter
DOI: 10.1594/pangaea.870793
title: Stretch tie points of ODP Site 154-928C
DOI: 10.1594/pangaea.774105
title: Hydrochemistry measured on water bottle samples during Bjarni Saemundsson cruise B14/2001
DOI: 10.1594/pangaea.798369
title: (Table 2) Aragonite content and stable oxygen isotopes of Globigerinoides ruber in ODP Hole 166-1006B sediments
DOI: 10.1594/pangaea.804032
title: (Table 1) Stable oxygen isotope ratios of Globigerinoides ruber from ODP Hole 164-994C sediments
DOI: 10.1594/pangaea.690304
title: Radiosonde M6_R052 during METEOR cruise M6 on 1966-08-30 05:28h

description: Height of tropause 10570 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.798370
title: (Table 3) Aragonite content, stable oxygen isotopes of Globigerinoides ruber, and age of ODP Site 166-1006 sediments

description: Sediment depth is given in mcd. For the creation of the age model, ODP Site 166-1006 oxygen isotope record was correlated to the Site 130-806 profile as provided by Berger et al. (1993, doi:10.2973/odp.proc.sr.130.023.1993) to facilitate low-latitude Atlantic-Pacific comparisons. The stable isotope record of ODP Site 130-806 was tuned by using the obliquity cycles apparent in the record (Berger et al., 1993, doi:10.2973/odp.proc.sr.130.023.1993).
DOI: 10.1594/pangaea.854306
title: Annotated record of the detailed examination of Mn deposits from “Michael Sars” North Atlantic Deep-Sea Expedition 1910

description: The deposit-samples and rock specimens brought home by the "Michael Sars" were received in the Challenger Office shortly after the return of the expedition, and upon examination the rock specimens proved to be so numerous and to offer so many points of interest that Dr. B. N. Peach, F. R. S., was requested to report upon them. A brief note on his results appeared in "The Depths of the Ocean" (London, Macmillan, 1912), pp. 202-209, and his detailed report was published in the Proc. Roy. Soc. Edin., vol. XXXII., pp. 262—291, 1912. When the author met Dr. Hjort in London in May 1914 he desired me to prepare, for publication in the series of Reports on the scientific Results of the "Michael Sars" North Atlantic Expedition, descriptions of the deposit samples, including for each station a brief summary of Dr. Peach's observations on the rock-specimens obtained. The accompanying Report shows that the "Michael Sars" expedition has made a notable contribution to our knowledge regarding the materials covering the floor of the North Atlantic Ocean.
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: Chumley, James (1932): Report on the deposit-samples collected during the "Michael Sars" North Atlantic Deep-Sea Expedition 1910. In: Report on the scientific results of the "Michael Sars" north Atlantic deep-sea expedition 1910, carried out under the auspices of the Norwegian government and the superintendence of Sir John Murray, K.C.B., and Dr. Johan Hjort. The Trustees of the Bergen museum, Bergen. Volume 1, 12 pp
DOI: 10.1594/pangaea.689256
title: Radiosonde M2_R296 during METEOR cruise M2 on 1965-11-19 05:31h

description: Height of tropause 16490 m; Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.744282
title: Physical oceanography during unknown cruise IYFS/USSR/1977 to the North Sea
DOI: 10.1594/pangaea.57021
title: (Table 3) Stable oxygen isotope ratios of Uvigerina spp. from DSDP Hole 75-532

description: isotopic measurements: N.J. Shackleton, Godwin Laboratory, Cambridge
DOI: 10.6084/m9.figshare.24585909
title: Additional file 1 of Different equations for estimating age-related changes of glomerular filtration rate in the healthy population

description: Additional file 1: Figure S1. Bland-Altman plot for eGFRs by different equations comparisons according to age in the males. Differences were plotted between eGFR by two of CKD-EPI, FAS, and Xiangya equations in male participants aged (A) 18-29 years, (B) 30-39 years, (C) 40-49 years, (D) 50-59 years, (E) 60-69 years, and (F) ≥70 years. The blue solid line represents the mean of the differences. The red dashed line indicates 1.96 standard deviations around the mean differences. CKD-EPI: chronic kidney disease epidemiology collaboration equation based on serum creatinine; FAS: full age spectrum based on serum creatinine and age. Figure S2. Bland-Altman plot for eGFRs by different equations comparisons according to age in the females. Differences were plotted between eGFR by two of CKD-EPI, FAS, and Xiangya equations in female participants aged (A) 18-29 years, (B) 30-39 years, (C) 40-49 years, (D) 50-59 years, (E) 60-69 years, and (F) ≥70 years. The blue solid line represents the mean of the differences. The red dashed line indicates 1.96 standard deviations around the mean differences. CKD-EPI: chronic kidney disease epidemiology collaboration equation based on serum creatinine; FAS: full age spectrum based on serum creatinine and age. Figure S3. Scatter plot of difference between two of CKD-EPI, FAS, and Xiangya equations with increasing serum creatinine. Difference between eGFR by different equations of each individual is shown as black plot in total population, dark blue plot in the males, and orange plot in the females. The fitting line is shown as dark blue solid line in the males and orange solid line in the females. eGFR: estimated glomerular filtration rate; CKD-EPI: chronic kidney disease epidemiology collaboration equation based on serum creatinine; FAS: full age spectrum based on serum creatinine and age.
DOI: 10.6084/m9.figshare.24585909.v1
title: Additional file 1 of Different equations for estimating age-related changes of glomerular filtration rate in the healthy population

description: Additional file 1: Figure S1. Bland-Altman plot for eGFRs by different equations comparisons according to age in the males. Differences were plotted between eGFR by two of CKD-EPI, FAS, and Xiangya equations in male participants aged (A) 18-29 years, (B) 30-39 years, (C) 40-49 years, (D) 50-59 years, (E) 60-69 years, and (F) ≥70 years. The blue solid line represents the mean of the differences. The red dashed line indicates 1.96 standard deviations around the mean differences. CKD-EPI: chronic kidney disease epidemiology collaboration equation based on serum creatinine; FAS: full age spectrum based on serum creatinine and age. Figure S2. Bland-Altman plot for eGFRs by different equations comparisons according to age in the females. Differences were plotted between eGFR by two of CKD-EPI, FAS, and Xiangya equations in female participants aged (A) 18-29 years, (B) 30-39 years, (C) 40-49 years, (D) 50-59 years, (E) 60-69 years, and (F) ≥70 years. The blue solid line represents the mean of the differences. The red dashed line indicates 1.96 standard deviations around the mean differences. CKD-EPI: chronic kidney disease epidemiology collaboration equation based on serum creatinine; FAS: full age spectrum based on serum creatinine and age. Figure S3. Scatter plot of difference between two of CKD-EPI, FAS, and Xiangya equations with increasing serum creatinine. Difference between eGFR by different equations of each individual is shown as black plot in total population, dark blue plot in the males, and orange plot in the females. The fitting line is shown as dark blue solid line in the males and orange solid line in the females. eGFR: estimated glomerular filtration rate; CKD-EPI: chronic kidney disease epidemiology collaboration equation based on serum creatinine; FAS: full age spectrum based on serum creatinine and age.
DOI: 10.1594/pangaea.696298
title: Concentrations of organic carbon, nitrogen and phosphorus in waters of the tropical North Atlantic at Station POS284-169
DOI: 10.1594/pangaea.663428
title: Oceanography at CTD/bottle station IFREMER_0268
DOI: 10.1594/pangaea.665632
title: Oceanography at CTD/bottle station IFREMER_2472
DOI: 10.1594/pangaea.665773
title: Oceanography at CTD/bottle station IFREMER_2599
DOI: 10.1594/pangaea.753123
title: Basic measurements of radiation at station Chesapeake Light (2010-09)
DOI: 10.1594/pangaea.689541
title: Radiosonde M49_R164 during METEOR cruise M49 on 1978-08-16 22:18h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.761627
title: (Table 1) Distribution of planktonic foraminifera in the latest Pliocene to Holocene section of ODP Hole 149-897A

description: Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present.
DOI: 10.1594/pangaea.689459
title: Radiosonde M49_R078 during METEOR cruise M49 on 1978-07-31 08:46h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.689527
title: Radiosonde M49_R150 during METEOR cruise M49 on 1978-08-07 16:16h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de