cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.874240
title: RAFOS Float Data in the Northeast Atlantic 1997-2003 from the SFB460 Project

description: This data collection contains RAFOS float trajectories from the Northeast Atlantic, in and around the Iceland Basin, collected at depths of 1500 m and 2600 m. The data are from the time period 1997-2003 and were collected as part of the project "Sonderforschungsbereich 460 (SFB460)", funded by the German "Deutsche Forschungsgemeinschaft". The data are presented in two versions: one version contains the full time series with possible gaps in the trajectories whenever the RAFOS tracking system was unavailable (see "Download data"), and the other version has gaps removed/interpolated and has been subjected to a smoothing filter (see "Other version"). Further details are available in a report that is included with this data collection as well (see "Further details").
DOI: 10.1594/pangaea.874295
title: (Table S4) Summary of published (Suganuma and Ogg, 2006, 2006) and new (this study; Edgar et al., 2007) samples run to establish palaeomagnetic stratigraphy of ODP Hole 207-1260B

description: Characteristic direction polarity ratings: N or R = well-defined directions computed from at least three vectors, NP or RP - less precise directions computed from only two vectors or a suite of vectors or a suite of vectors displaying high dispersion, NPP or RPP = samples that did not achieve adequate cleaning during demagnetization but their polarity was obvious N?? or R?? = uncertain, INT = indeterminate.
DOI: 10.1594/pangaea.875747
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 85 (Holes 572D, 573D, 574D )

description: SDP Leg 85 was designed to take advantage of a new hydraulic piston corer (HPC) enabling to recover fairly undisturbed samples from the upper 100 to 300 m and thus to carry out high resolution stratigraphic studies. The JOIDES Ocean Paleoenvironment Panel selected five drill sites, two sites (571 and 572) are in the eastern Pacific, and the three others (573, 574, and 575) form a north-south line that lies at approximately 133°W across the equatorial high productivity zone.
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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.
DOI: 10.1594/pangaea.875089
title: Annotated record of the detailed examination of Mn deposits from the 1993 R/V Sonne SO-84 expedition in the Atlantic Ocean

description: The SO-84 cruise from Las Palmas to Cape Town studied the underwater volcanism associated with the St Helena hotspot. Wide-spaced grid mapping of a region south and west of St Helena island identified three previously unknown hotspot volcanoes (which we named Josephine 16°27'S-9°W, Jade 16°13'S-7°46'W and Benjamin 16°12'S-8°31'W) and several older, probably near-ridge-generated seamounts. The newly discovered hotspot seamounts, and the previously-known seamounts of Bagration, Bonaparte and Kutuzov were mapped and sampled. Onboard geochemical studies confirm that they all show trace-element (Rb, Nb, Y, Zr, Sr) enriched, hotspot magma-type compositions. Morphological studies and the state of the samples collected from the seamounts (all have at least 1 mm-thick Mn crusts) suggest that none of the volcanoes is presently active, and that the St Helena hotspot is probably extinct at the present time. Josephine appears to be the youngest volcano, and one dredge here yielded fossil hydrothermal material (Fe-hydroxides). To test the hypothesis that the extinction of the hotspot is due to its magmas being channelled to the Mid-Atlantic Ridge, several dredges were taken on the ridge opposite St Helena. Furthermore, in the proposed influence zone of the St Helena plume head, Grattan seamount (9°44'S-12°48'W) was also sampled to examine whether its composition has been affected by the St Helena plume. During the transit from Las Palmas to St Helena, several sediment cores were taken in 3000 m water depth close to the ridge axis for palaeoclimatological work.
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: Devey, Colin W; Ackermand, Dietrich; Binard, Nicolas; Chmarzynski, P; Franke-Bruckmaier, B; Geldmacher, Jörg; Graupner, T; Haake, F W; Haase, Karsten M; Hemond, Christophe; Krüger, O; Mühlhan, Norbert; O'Connor, John; Ott, S; Peucker-Ehrenbrink, Bernhard; Pototzki, Frank; Segl, Monika; Tichomirov, W (1993): Cruise report SO-84: The St Helena hotspot - Las Palmas-Cape Town 02.01.93-20.02.93. Berichte - Reports, Geologisch-Paläontologisches Institut und Museum, Christian-Albrechts-Universität, Kiel; 64; 1-103; ISSN 0175-9302, TIB - Technische Informationsbibliothek Universitätsbibliothek Hannover, Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 64, 103 pp
DOI: 10.1594/pangaea.875764
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 92 (Holes 597, 597C, 598, 600, 600B, 600C, 601, 601B, 602B)

description: The realization that ridgecrest hydrothermal activity is more common along the faster spreading centers of the Pacific Ocean than along the slowly spreading Mid- Atlantic Ridge has given rise to a generally accepted correlation between the intensity of this activity and seafloor spreading rate. Knowledge of seafloor hydrothermal activity is essential to our understanding of the oceanic cycling of elements, and an understanding of the history of hydrothermal activity is important to ocean paleochemistry and many other aspects of the history of the Earth and the oceans. Leg 92 was undertaken primarily to determine the nature and history of basalt-seawater (or hydrogeology) interactions at and on the flanks of the East Pacific Rise (EPR).
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.
DOI: 10.1594/pangaea.875570
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 82 (Holes 556, 558, 559, 562, 563, 564)

description: One of the most important geologic discoveries of the 1960s was the remarkable uniformity of the basalts produced at mid-ocean ridges. These basalts have a markedly different tholeiitic composition compared to the alkalic basalts from ocean islands. But very little is known about temporal variations in the composition of basalts derived from one or several mantle sources associated with both normal and anomalously shallow sections of the mid-ocean ridges. The strategy for drilling on DSDP Leg 82 was to set up a broad grid encompassing all possible drilling sites west and southwest of the present Azores Triple Junction in order to investigate these problems.
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.
DOI: 10.1594/pangaea.871010
title: Spliced magnetic susceptibility of ODP Site 154-926
DOI: 10.1594/pangaea.876695
title: CTD data Kiel276-19
DOI: 10.1594/pangaea.874296
title: (Table S5) Magnetochron datum table for ODP Hole 207-1260B
DOI: 10.1594/pangaea.875753
title: Annotated record of the detailed examination of Mn deposits from DSDP Leg 87 (Holes 582B, 583, 583A, 583D, 583E, 583F, 584)

description: The DSDP Leg 87 expedition was dedicated to drilling active margins and was designed to investigate two very different regions: the Nankai Trough and the Japan Trench. The broad objective was to study the location, directions, and rates of lithospheric plate convergence for this active margin zone off Japan.
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.
DOI: 10.1594/pangaea.876688
title: CTD data Kiel276-13
DOI: 10.1594/pangaea.879377
title: Upper Miocene-Lower Pliocene nannofossil taxonomy and stratigraphy of ODP Site 154-926, 154-928 and 154-929, 21302-23293 ka

description: # = reworked
DOI: 10.1594/pangaea.879226
title: Remote sensing reflectance during POLARSTERN cruise ANT-XXVI/4

description: In the previous remote sensing reflectance (RRS) data sets , the RRS data were not correctly calculated because the input upwelling radiance (Lu) data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement. While the effect of this mistake is low were the downwelling irradiance changes slowly with wavelength it becomes strong were it changes quickly which is below 430 nm. In the now submitted data the correct wavelengths for Lu data have been used for the calculations. The results of the publications related to these data were not affected - we had used both versions of RRS data and got the same results since in these studies the errorneous features &lt;430 nm are consistent and are neither used for the hierarchical cluster analysis (only data &gt;430 nm are considered) performed in Taylor et al. 2011 (doi:10.5194/bg-8-3609-2011) nor for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015 (doi:10.5194/os-11-139-2015).
DOI: 10.1594/pangaea.879297
title: Upper Miocene-Lower Pliocene nannofossil taxonomy and stratigraphy of ODP Site 154-926, 5507-7485 ka

description: # = reworked
DOI: 10.1594/pangaea.879327
title: Upper Miocene-Lower Pliocene nannofossil taxonomy and stratigraphy of ODP Site 154-926, 9705-12493 ka

description: # = reworked
DOI: 10.1594/pangaea.879334
title: Upper Miocene-Lower Pliocene nannofossil taxonomy and stratigraphy of ODP Site 154-926, 7517-9692 ka

description: # = reworked
DOI: 10.1594/pangaea.879355
title: Upper Miocene-Lower Pliocene nannofossil taxonomy and stratigraphy of ODP Sites 154-925 and 154-126, 12534-13833 ka

description: # = reworked
DOI: 10.1594/pangaea.876699
title: CTD data Kiel276-22
DOI: 10.1594/pangaea.879357
title: Upper Miocene-Lower Pliocene nannofossil taxonomy and stratigraphy of ODP Sites 154-925 and 154-926, 13756-15899 ka

description: # = reworked
DOI: 10.1594/pangaea.876703
title: CTD data Kiel276-26
DOI: 10.1594/pangaea.879411
title: Upwelling spectral radiance as measured in different depths at radiometer station PS75/283-4 (corrected version)

description: In the previous upwelling radiance (Lu) profile data set (doi:10.1594/PANGAEA.821182), Lu data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement). The results of the publications related to these data were not affected. Taylor et al. 2013 investigated only Lu data incorrectly shifted by 3 nm, so the analysis was consistent within itself. Bracher et al. 2015 used the remote sensing reflectance (RRS) data calculated from the incorrectly shifted Lu data. The resulting RRS data only showed inconsistencies were the incoming downwelling irradiance changes quickly with wavelengths, which resulted erroneous features &lt;430 nm. We have used both versions (previous and the one presented here) Lu and RRS data and got the same results since the wrong features &lt;430 nm are consistent and are not used for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015.
DOI: 10.1594/pangaea.876704
title: CTD data Kiel276-27
DOI: 10.1594/pangaea.879418
title: Upwelling spectral radiance as measured in different depths at radiometer station PS75/295-5 (corrected version)

description: In the previous upwelling radiance (Lu) profile data set (doi:10.1594/PANGAEA.821189), Lu data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement). The results of the publications related to these data were not affected. Taylor et al. 2013 investigated only Lu data incorrectly shifted by 3 nm, so the analysis was consistent within itself. Bracher et al. 2015 used the remote sensing reflectance (RRS) data calculated from the incorrectly shifted Lu data. The resulting RRS data only showed inconsistencies were the incoming downwelling irradiance changes quickly with wavelengths, which resulted erroneous features &lt;430 nm. We have used both versions (previous and the one presented here) Lu and RRS data and got the same results since the wrong features &lt;430 nm are consistent and are not used for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015.
DOI: 10.1594/pangaea.872510
title: (Supplement Table S9) Age model of ODP Site 154-926
DOI: 10.1594/pangaea.879436
title: Upwelling spectral radiance as measured in different depths at radiometer station PS73/030-2 (corrected version)

description: In the previous upwelling radiance (Lu) profile data set (doi:10.1594/PANGAEA.820803), Lu data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement). The results of the publications related to these data were not affected. Taylor et al. 2013 investigated only Lu data incorrectly shifted by 3 nm, so the analysis was consistent within itself. Taylor et al. 2011 and Bracher et al. 2015 used the remote sensing reflectance (RRS) data calculated from the incorrectly shifted Lu data. The resulting RRS data only showed inconsistencies were the incoming downwelling irradiance changes quickly with wavelengths, which resulted erroneous features &lt;430 nm. We have used both versions (previous and the one presented here) Lu and RRS data and got the same results since the wrong features &lt;430 nm are consistent and are neither used for the hierarchical cluster analysis (only data &gt;430 nm are considered) performed in Taylor et al. 2011 nor for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015.
DOI: 10.1594/pangaea.879439
title: Upwelling spectral radiance as measured in different depths at radiometer station PS73/036-2 (corrected version)

description: In the previous upwelling radiance (Lu) profile data set (doi:10.1594/PANGAEA.820806), Lu data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement). The results of the publications related to these data were not affected. Taylor et al. 2013 investigated only Lu data incorrectly shifted by 3 nm, so the analysis was consistent within itself. Taylor et al. 2011 and Bracher et al. 2015 used the remote sensing reflectance (RRS) data calculated from the incorrectly shifted Lu data. The resulting RRS data only showed inconsistencies were the incoming downwelling irradiance changes quickly with wavelengths, which resulted erroneous features &lt;430 nm. We have used both versions (previous and the one presented here) Lu and RRS data and got the same results since the wrong features &lt;430 nm are consistent and are neither used for the hierarchical cluster analysis (only data &gt;430 nm are considered) performed in Taylor et al. 2011 nor for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015.
DOI: 10.1594/pangaea.879417
title: Upwelling spectral radiance as measured in different depths at radiometer station PS75/294-4 (corrected version)

description: In the previous upwelling radiance (Lu) profile data set (doi:10.1594/PANGAEA.821188), Lu data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement). The results of the publications related to these data were not affected. Taylor et al. 2013 investigated only Lu data incorrectly shifted by 3 nm, so the analysis was consistent within itself. Bracher et al. 2015 used the remote sensing reflectance (RRS) data calculated from the incorrectly shifted Lu data. The resulting RRS data only showed inconsistencies were the incoming downwelling irradiance changes quickly with wavelengths, which resulted erroneous features &lt;430 nm. We have used both versions (previous and the one presented here) Lu and RRS data and got the same results since the wrong features &lt;430 nm are consistent and are not used for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015.
DOI: 10.1594/pangaea.879420
title: Upwelling spectral radiance as measured in different depths at radiometer station PS75/297-3 (corrected version)

description: In the previous upwelling radiance (Lu) profile data set (doi:10.1594/PANGAEA.821191), Lu data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement). The results of the publications related to these data were not affected. Taylor et al. 2013 investigated only Lu data incorrectly shifted by 3 nm, so the analysis was consistent within itself. Bracher et al. 2015 used the remote sensing reflectance (RRS) data calculated from the incorrectly shifted Lu data. The resulting RRS data only showed inconsistencies were the incoming downwelling irradiance changes quickly with wavelengths, which resulted erroneous features &lt;430 nm. We have used both versions (previous and the one presented here) Lu and RRS data and got the same results since the wrong features &lt;430 nm are consistent and are not used for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015.
DOI: 10.1594/pangaea.879424
title: Upwelling spectral radiance as measured in different depths at radiometer station PS75/285-4 (corrected version)

description: In the previous upwelling radiance (Lu) profile data set (doi:10.1594/PANGAEA.821183), Lu data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement). The results of the publications related to these data were not affected. Taylor et al. 2013 investigated only Lu data incorrectly shifted by 3 nm, so the analysis was consistent within itself. Bracher et al. 2015 used the remote sensing reflectance (RRS) data calculated from the incorrectly shifted Lu data. The resulting RRS data only showed inconsistencies were the incoming downwelling irradiance changes quickly with wavelengths, which resulted erroneous features &lt;430 nm. We have used both versions (previous and the one presented here) Lu and RRS data and got the same results since the wrong features &lt;430 nm are consistent and are not used for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015.
DOI: 10.15468/dl.szbrck
title: Occurrence Download

description: A dataset containing 187 species occurrences available in GBIF matching the query:
{
 "Geometry" : [
 "MULTIPOLYGON (((147.15677 -33.968242, 147.161262 -33.968242, 147.161262 -33.96375, 147.15677 -33.96375, 147.15677 -33.968242)), ((147.15677 -33.968242, 147.154525 -33.968242, 147.154525 -33.970488, 147.143296 -33.970488, 147.143296 -33.974979, 147.152279 -33.974979, 147.152279 -33.979471, 147.15677 -33.979471, 147.15677 -33.981717, 147.154525 -33.981717, 147.154525 -33.983962, 147.161262 -33.983962, 147.161262 -33.981717, 147.163508 -33.981717, 147.163508 -33.979471, 147.165754 -33.979471, 147.165754 -33.972733, 147.170245 -33.972733, 147.170245 -33.977225, 147.174737 -33.977225, 147.174737 -33.974979, 147.179228 -33.974979, 147.179228 -33.972733, 147.181474 -33.972733, 147.181474 -33.970488, 147.188212 -33.970488, 147.188212 -33.968242, 147.185966 -33.968242, 147.185966 -33.96375, 147.176983 -33.96375, 147.176983 -33.970488, 147.172491 -33.970488, 147.172491 -33.968242, 147.161262 -33.968242, 147.161262 -33.970488, 147.15677 -33.970488, 147.15677 -33.968242)))"
 ]
}

 The dataset includes 187 records from 9 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0070092-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.879225
title: Remote sensing reflectance during POLARSTERN cruise ANT-XXV/1

description: In the previous remote sensing reflectance (RRS) data sets , the RRS data were not correctly calculated because the input upwelling radiance (Lu) data were wrongly shifted by 3 nm (which responds to the originally resolution of the measurement. While the effect of this mistake is low were the downwelling irradiance changes slowly with wavelength it becomes strong were it changes quickly which is below 430 nm. In the now submitted data the correct wavelengths for Lu data have been used for the calculations. The results of the publications related to these data were not affected - we had used both versions of RRS data and got the same results since in these studies the errorneous features &lt;430 nm are consistent and are neither used for the hierarchical cluster analysis (only data &gt;430 nm are considered) performed in Taylor et al. 2011 (doi:10.5194/bg-8-3609-2011) nor for the pigment predictions (since these features are contained in the first empirical orthogonal function) in Bracher et al. 2015 (doi:10.5194/os-11-139-2015).
DOI: 10.1594/pangaea.871472
title: Table S46 - 405-kyr eccentricity cycle age model for ODP Site 207-1258 and Site 208-1263