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

description: A dataset containing 1230401 species occurrences available in GBIF matching the query:
{
 "and" : [
 "GadmGid is CHL.16_1",
 "OccurrenceStatus is Present"
 ]
}

 The dataset includes 1230401 records from 482 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0037406-250525065834625/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.djxgwd
title: Occurrence Download

description: A dataset listing the 277 species recorded in GBIF matching the query:
{
 "and" : [
 "Geometry MULTIPOLYGON(((170.67037 -45.8262,170.67048 -45.82645,170.67153 -45.82866,170.67178 -45.82915,170.67227 -45.83011,170.68077 -45.84132,170.69341 -45.85043,170.70053 -45.85326,170.70209 -45.85417,170.70513 -45.85509,170.7092 -45.85671,170.71051 -45.85693,170.71045 -45.85704,170.71107 -45.8572,170.7148 -45.85803,170.71882 -45.85925,170.73692 -45.86084,170.73709 -45.86082,170.73727 -45.86082,170.7379 -45.86081,170.73938 -45.86058,170.74016 -45.86062,170.74199 -45.86062,170.7439 -45.86059,170.74397 -45.86059,170.74424 -45.86059,170.7455 -45.86053,170.74697 -45.86051,170.74823 -45.86046,170.74932 -45.86032,170.75162 -45.86013,170.7519 -45.8601,170.75187 -45.85998,170.76563 -45.85815,170.78148 -45.85261,170.78254 -45.8521,170.78939 -45.84732,170.79005 -45.84782,170.79059 -45.84747,170.79339 -45.84453,170.799 -45.84062,170.79916 -45.84047,170.79787 -45.83984,170.80711 -45.83014,170.80713 -45.83012,170.81098 -45.81754,170.80966 -45.80546,170.81003 -45.80379,170.80629 -45.78909,170.79588 -45.77605,170.79587 -45.77604,170.78132 -45.76674,170.76344 -45.76095,170.76343 -45.76095,170.76193 -45.76081,170.75663 -45.75921,170.75232 -45.75893,170.74802 -45.75796,170.74191 -45.75798,170.7405 -45.75766,170.73909 -45.75757,170.73437 -45.75737,170.73349 -45.75736,170.71823 -45.75841,170.71698 -45.7586,170.70396 -45.76166,170.70361 -45.76178,170.68456 -45.77115,170.68408 -45.7715,170.67734 -45.77762,170.67543 -45.779,170.66669 -45.79116,170.66355 -45.80459,170.6663 -45.81807,170.66646 -45.81844,170.66692 -45.81947,170.66799 -45.82174,170.66914 -45.82397,170.67037 -45.8262)))",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is one of (Insecta, Arachnida, Onychophora, Athoracophoridae, Rhytididae)"
 ]
}

 The dataset's 277 records were derived from 12 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0003539-250415084134356/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.902267
title: (Figure 5) δ11B of early Holocene coralline algae from the Mediterranean Sea
DOI: 10.1594/pangaea.689847
title: Radiosonde M58_R023 during METEOR cruise M58 on 1981-09-20 10:56h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.786047
title: XRF-core logger measurements from IODP Hole 333-C0012G

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.913774
title: Relative abundances of dead planktonic foraminifera in surface sediments from the Barents Sea
DOI: 10.1594/pangaea.882147
title: Physical oceanography on section MVP_2015003_03 during CCGS Amundsen cruise MVP_2015003
DOI: 10.1594/pangaea.716796
title: (Table 1) Observed and initial Sr-Nd-Pb isotope ratios of basalts from the Caribbean Large Igneous Province

description: Sample positions are etimated from map, except ODP samples
DOI: 10.1594/pangaea.910554
title: Supplementary Table 1: Constitutive parameters from rate-and-state friction modeling of velocity step data
DOI: 10.1594/pangaea.882148
title: Physical oceanography on section MVP_2015003_04 during CCGS Amundsen cruise MVP_2015003
DOI: 10.1594/pangaea.913824
title: Magnetic hysteresis data of sediment core SWERUS-C3-L2-13-PC
DOI: 10.1594/pangaea.691422
title: Mesozooplankton average mass during Professor Vodyanitskiy cruise PV11, Part I

description: Mesozooplankton was sampled by open-closing JUDAY net with a 36 cm ring diameter and mesh sizes of 125 µm. The open-closing mechanism used was the Nansen mechanical lock system allowing nets to be vertically towed through standard depths (0-10, 10-25, 25-50, 50-100, 100-200, 200-300 m) and closed at the upper depth level. Integrated hauls (0-100, 100-200 m) were also taken. Depth of tow was evaluated by wire paid out and the angle of wire inclination. The 10-20 ml samples were preserved in 3-4% buffered formaldehyde and processed on return to the laboratory. All of copepods were identified to genus level, other taxanomic groups - to type, class, order and family levels.
DOI: 10.1594/pangaea.906206
title: Magnetic susceptibility of sediment core XC-01-2
DOI: 10.1594/pangaea.882145
title: Physical oceanography on section MVP_2015003_01 during CCGS Amundsen cruise MVP_2015003
DOI: 10.1594/pangaea.716801
title: (Appendix Table 2) Trace element concentrations of basalts from the Caribbean Large Igneous Province

description: Sample positions are etimated from map, except ODP samples
DOI: 10.1594/pangaea.910574
title: Table 2. Southern Hikurangi SSE parameters

description: Vo = initial slip velocity (cm/yr), r = downdip half width (km), Mw = moment magnitude
DOI: 10.1594/pangaea.762371
title: Current measurements with ADCP 20030717_StMartin

description: Current measurements were acquired from several stations around the Cap de la Hague over periods of 14-25 hours, using a SONTEK ADP profiler with a frequency of 1 000 kHz placed on the seabed. Current profiles were collected every 15 s, with vertical resolution of 2 m. files contains average speeds from surface to bottom.
DOI: 10.1594/pangaea.785975
title: (Table T1) Calcium carbonate mineralogy and stable isotopic composition of ODP Hole 182-1127B
DOI: 10.1594/pangaea.762377
title: Current measurements with ADCP 20050404_Ecalgrain

description: Current measurements were acquired from several stations around the Cap de la Hague over periods of 14-25 hours, using a SONTEK ADP profiler with a frequency of 1 000 kHz placed on the seabed. Current profiles were collected every 15 s, with vertical resolution of 2 m. files contains average speeds from surface to bottom.
DOI: 10.1594/pangaea.689840
title: Radiosonde M58_R015 during METEOR cruise M58 on 1981-09-18 17:00h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.689841
title: Radiosonde M58_R016 during METEOR cruise M58 on 1981-09-18 20:17h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.689887
title: Radiosonde M58_R066 during METEOR cruise M58 on 1981-09-27 08:02h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.706182
title: (Table 2) Stable isotope data (δ¹³C and δ¹⁸O) and temperature estimates for carbonate-rich samples and carbonate nodules from ODP Hole 168-1032A

description: Temperature range calculated for equilibrium with porewaters with d18O of -1% to 0.5%.
DOI: 10.1594/pangaea.689888
title: Radiosonde M58_R067 during METEOR cruise M58 on 1981-09-27 10:58h

description: Data processing by Wolfgang Gloeden, Maritime Klimaüberwachung (KU24), Deutscher Wetterdienst, http://www.dwd.de
DOI: 10.1594/pangaea.745635
title: Statistics for grain size analysis of surface sediments off Sylt collected during HEINCKE cruise HE258
DOI: 10.1594/pangaea.802900
title: (Table 4) Calcareous nannofossil datums of ODP Hole 165-999A

description: Sediment depth is given in mbsf. The ages of nannofossil datums and bioevents were taken from Raffi and Flores (1995, doi:10.2973/odp.proc.sr.138.112.1995) for the Miocene to lower Pliocene and Takayama et al. (1995) for the upper Pliocene and Pleistocene.
DOI: 10.1594/pangaea.913847
title: Mg/Ca ratios of Oridorsalis umbonatus, and Bottom Water reconstruction for ODP Site 199-1218

description: Mg/Ca analysed on Oridorsalis umbonatus at IMCS, Rutgers University
DOI: 10.1594/pangaea.730163
title: (Table 20) Chemical composition of medium-grained basalt from the California Gulf, DSDP Hole 65-483
DOI: 10.1594/pangaea.913848
title: Sea water stable oxygen isotope rconstruction for ODP Site 199-1218
DOI: 10.1594/pangaea.762369
title: Current measurements with ADCP 20030614_Omonville

description: Current measurements were acquired from several stations around the Cap de la Hague over periods of 14-25 hours, using a SONTEK ADP profiler with a frequency of 1 000 kHz placed on the seabed. Current profiles were collected every 15 s, with vertical resolution of 2 m. files contains average speeds from surface to bottom.
DOI: 10.1594/pangaea.906217
title: Organic geochemistry of sediment core XC-01-2
DOI: 10.1594/pangaea.820711
title: A return-on-investment framework to identify conservation priorities in Africa

description: Environmental conservation activities must continue to become more efficient and effective, especially in Africa where development and population growth pressures continue to escalate. Recently, prioritization of conservation resources has focused on explicitly incorporating the economic costs of conservation along with better defining the outcomes of these expenditures. We demonstrate how new global and continental data that spans social, economic, and ecological sectors creates an opportunity to incorporate return-on-investment (ROI) principles into conservation priority setting for Africa. We suggest that combining conservation priorities that factor in biodiversity value, habitat quality, and conservation management investments across terrestrial, freshwater, and coastal marine environments provides a new lens for setting global conservation priorities. Using this approach we identified seven regions capturing interior and coastal resources that also have high ROI values that support further investment. We illustrate how spatially explicit, yet flexible ROI analysis can help to better address uncertainty, risk, and opportunities for conservation, while making values that guide prioritization more transparent. In one case the results of this prioritization process were used to support new conservation investments. Acknowledging a clear research need to improve cost information, we propose that adopting a flexible ROI framework to set conservation priorities in Africa has multiple potential benefits.
description: ROV (sprint 103) equiped with 36mm still and two viedo cameras. Still photographs: Kodak Ektachrome 100; Nikon super coolscan 4000ED; JPEG compression.
description: Supplement to: Tear, Timothy H; Stratton, Bradford N; Game, Edward T; Brown, Matthew T; Apse, Colin D; Shirer, Rebecca R (2014): A return-on-investment framework to identify conservation priorities in Africa. Biological Conservation, 173, 42-52
DOI: 10.1594/pangaea.833752
title: Spatial database of canopy plant densities created from satellite images over Galapagos in 2011, with intent to manage invasive species

description: Mapping is an important tool for the management of plant invasions. If landscapes are mapped in an appropriate way, results can help managers decide when and where to prioritize their efforts. We mapped vegetation with the aim of providing key information for managers on the extent, density and rates of spread of multiple invasive species across the landscape. Our case study focused on an area of Galapagos National Park that is faced with the challenge of managing multiple plant invasions. We used satellite imagery to produce a spatially-explicit database of plant species densities in the canopy, finding that 92% of the humid highlands had some degree of invasion and 41% of the canopy was comprised of invasive plants. We also calculated the rate of spread of eight invasive species using known introduction dates, finding that species with the most limited dispersal ability had the slowest spread rates while those able to disperse long distances had a range of spread rates. Our results on spread rate fall at the lower end of the range of published spread rates of invasive plants. This is probably because most studies are based on the entire geographic extent, whereas our estimates took plant density into account. A spatial database of plant species densities, such as the one developed in our case study, can be used by managers to decide where to apply management actions and thereby help curtail the spread of current plant invasions. For example, it can be used to identify sites containing several invasive plant species, to find the density of a particular species across the landscape or to locate where native species make up the majority of the canopy. Similar databases could be developed elsewhere to help inform the management of multiple plant invasions over the landscape.
description: Spatial data are provided in ESRI shapefile format (zipped) in geographic coordinates and using the datum WGS 1984. Explanatory notes are provided in an Excel workbook, along with canopy plant density data that can be manipulated and/or joined with the attribute table of the ESRI shapefile. Methodology is described in the Neobiota publication.
description: Supplement to: Trueman, Mandy; Standish, Rachel; Orellana, Daniel; Cabrera, Wilson (2014): Mapping the extent and spread of multiple plant invasions can help prioritise management in Galapagos National Park. NeoBiota, 23, 1-16
DOI: 10.1594/pangaea.762374
title: Current measurements with ADCP 20030809_Vauville

description: Current measurements were acquired from several stations around the Cap de la Hague over periods of 14-25 hours, using a SONTEK ADP profiler with a frequency of 1 000 kHz placed on the seabed. Current profiles were collected every 15 s, with vertical resolution of 2 m. files contains average speeds from surface to bottom.
DOI: 10.1594/pangaea.864922
title: Annotated record of the detailed examination of Mn deposits from T3 Ice Island in the Arctic Ocean

description: The cores described were taken by the personnel of the Lamont-Doherty Earth Observatory (LDEO) on the T3 Antarctic Ice Island in the Arctic Ocean from 1953 until 1969. The recovered cores are available at Lamont-Doherty Earth Observatory 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: Lamont-Doherty Earth Observatory (1969): T3 Antarctic Ice Island - Descriptions of Cores. Lamont Geological Observatory, Columbia University, New York, unpublished
DOI: 10.1594/pangaea.748439
title: Meteorological observations during DANAE cruise from Cape Clear to Carlise Bay started at 1761-03-12
DOI: 10.1594/pangaea.750743
title: Meteorological observations during MERCUUR cruise from Curacao to Puerto Cabello started at 1820-07-19
DOI: 10.1594/pangaea.746124
title: (Table 4) Chemistry of interstitial water of ODP Site 107-653
DOI: 10.1594/pangaea.751562
title: Meteorological observations during Prins Hendrik cruise from Sourabaija to Samarang started at 1848-08-17
DOI: 10.1594/pangaea.710762
title: (Table 3) Molecular and isotopic properties of hydrate-bound gases from ODP Site 204-1244

description: Gas concentrations are given as volume parts of natural gases. Zero values = not detected.
DOI: 10.1594/pangaea.728887
title: (Table 4) Abundance of silicoflagellates in ODP Hole 120-749B
DOI: 10.1594/pangaea.824524
title: Stable carbon isotope record of sediment core Ancora

description: The standard paradigm that the Paleocene/Eocene thermal maximum (PETM) represents a threshold event intrinsic to Earth's climate and connected in some way with long-term warming has influenced interpretations of the geochemical, climate, and biological perturbations that occurred at this event. As recent high-resolution data have demonstrated that the onset of the event was geologically instantaneous, attempts to account for the event solely through endogenous mechanisms have become increasingly strained. The rapid onset of the event indicates that it was triggered by a catastrophic event which we suggest was most likely a bolide impact. We discuss features of the PETM that require explanation and argue that mechanisms that have previously been proposed either cannot explain all of these features or would require some sort of high-energy trigger. A bolide impact could provide such a trigger and, in the event of a comet impact, could contribute directly to the shape of the carbon isotope curve. We introduce a carbon cycle model that would explain the PETM by global warming following a bolide impact, leading to the oxidation of terrestrial organic carbon stores built up during the late Paleocene. Our intention is to encourage other researchers to seriously consider an impact trigger for the PETM, especially in the absence of plausible alternative mechanisms.
description: Supplement to: Cramer, Benjamin S; Kent, Dennis V (2005): Bolide summer: The Paleocene/Eocene thermal maximum as a response to an extraterrestrial trigger. Palaeogeography, Palaeoclimatology, Palaeoecology, 224(1-3), 144-166
DOI: 10.1594/pangaea.477575
title: Hydrochemistry measured on water bottle samples at station SAtl_1983_OC_22S/65

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.749369
title: Meteorological observations during GALLARDO cruise from Cádiz to Cádiz started at 1779-06-22
DOI: 10.1594/pangaea.785524
title: (Figure 6) Distribution of middle Miocene to late Pliocene calcareous nannofossils in ODP Hole 132-810C

description: Sediment depth is given in mbsf. Species abundance: A = abundant (more than 1 specimen per field of view; 1250 X); C = common (at least 1 specimen in 10 fields of view); F = frequent (at least 1 specimen in 30 fields of view); R = rare (less than 1 specimen in 30 fields of view); RR = very rare (1 or 2 specimens detected during the analysis).
DOI: 10.1594/pangaea.762378
title: Current measurements with ADCP 20050410_Vauville

description: Current measurements were acquired from several stations around the Cap de la Hague over periods of 14-25 hours, using a SONTEK ADP profiler with a frequency of 1 000 kHz placed on the seabed. Current profiles were collected every 15 s, with vertical resolution of 2 m. files contains average speeds from surface to bottom.
DOI: 10.1594/pangaea.762381
title: Current measurements with ADCP 20050412_Omonville

description: Current measurements were acquired from several stations around the Cap de la Hague over periods of 14-25 hours, using a SONTEK ADP profiler with a frequency of 1 000 kHz placed on the seabed. Current profiles were collected every 15 s, with vertical resolution of 2 m. files contains average speeds from surface to bottom.
DOI: 10.1594/pangaea.477309
title: Hydrochemistry measured on water bottle samples at station NPac_1985_TT_47Na/5-1

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.913903
title: Mg-Ca ratios of benthic foraminifera and BWT reconstruction for ODP Site 130-806B
DOI: 10.1594/pangaea.719806
title: Radiosonde measurements from station Desert Rock (2007-02)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.719813
title: Ultra-violet measurements from station Desert Rock (2007-04)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-08.
DOI: 10.1594/pangaea.773394
title: Description of lithologic units (VCD) from IODP Hole 316-C0006D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.719814
title: Radiosonde measurements from station Desert Rock (2007-04)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.808020
title: (Figure 6) Radiolarian range chart of ODP Site 138-849, part II

description: DEPTH, sediment is given in mbsf. Relative abundance of individual species: R = rare (&lt;10 specimens); F = few, (10-100 specimens); C = common (100-200 specimens), and A = abundant (&gt;200 specimens). A- signifies that a species was looked for and not found, small case letters = specimens found that are thought to be reworked, ? = a dubious identification.
DOI: 10.1594/pangaea.739921
title: Pollen profile UBERLING, Grosses Überling Schattseit-Moor, Austria

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.719817
title: Ultra-violet measurements from station Desert Rock (2007-05)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-08.
DOI: 10.1594/pangaea.806774
title: (Table 1) Paleomagnetic reversal boundary depths of ODP Site 138-845

description: DEPTH, sediment is given in mbsf. The magnetic polarity time scale and nomenclature are from Cande and Kent (1992).
DOI: 10.1594/pangaea.719818
title: Radiosonde measurements from station Desert Rock (2007-05)

description: If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.725938
title: Flux data from trap CI2