cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.950158
title: Master track of Senckenberg SEN2212 cruise on 2022-05-03

description: Raw navigation data acquired by the navigation system of the Senckenberg during the expedition SEN2212 which took place on the 3rd of May 2022 between Jade and Wangerooge in the German North Sea coast. The track was acquired with a Hemisphere Cresent R131RCVR GPS antenna and recorded with the Ocean Floor Observation Protocol (OFOP) software. No further processing was undertaken. The data is provided as a master track with 1 sec resolution derived from the position sensors' data. This cruise was an activity of the CONMAR project of the DAM research mission "Protection and Sustainable Use of Marine Areas".
DOI: 10.15468/dl.63kvn5
title: Occurrence Download

description: A dataset containing 69565 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Gorsachius melanolophus (Raffles, 1822)"
 ]
}

 The dataset includes 69565 records from 66 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0011584-241024112534372/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.957081
title: Multibeam bathymetry raw data (Kongsberg EM710 entire dataset) of RV METEOR during cruise M156

description: Raw multibeam bathymetry data were recorded on RV METEOR during M156 using Kongsberg EM710 multibeam echosounder. The cruise took place between 2019-07-03 - 2019-08-01, (Mindelo-Mindelo, Cape Verde) in the Atlantic Ocean. Data were recorded within Cabo Verde & Mauritanian EEZ and throughout the whole time spend outside EEZs with an approximate average depth of around 2000m.To enhance MBES data accuracy, CTD casts were made in the working area prior to each MBES survey using CTD rosette to raytrace beams with the obtained sound velocity profiles (SVP). During transits, real-time measurement by SV-Profiler at transducer depth were directly applied during acquisition with SIS Seafloor Information System.Data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors can be expected due to the lack of proper SVP.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH, thus SVP files are added to this dataset.Data acquisition and provision were accomplished within work package 2 of the EU Horizon 2020 project iAtlantic- Integrated Assessment of Atlantic Marine Ecosystem in Space and Time (https://www.iatlantic.eu/) IceAge project.
description: These data should not be used for navigational purposes.
DOI: 10.1594/pangaea.957082
title: Multibeam bathymetry raw data (Kongsberg EM122 entire dataset) of RV METEOR during cruise M156

description: Raw multibeam bathymetry data were recorded on RV METEOR during M156 using Kongsberg EM122 multibeam echosounder. The cruise took place between 2019-07-03 - 2019-08-01, (Mindelo-Mindelo, Cape Verde) in the Atlantic Ocean. Data were recorded within Cabo Verde & Mauritanian EEZ and throughout the whole time spend outside EEZs with an approximate average depth of around 2000m.To enhance MBES data accuracy, CTD casts were made in the working area prior to each MBES survey using CTD rosette to raytrace beams with the obtained sound velocity profiles (SVP). During transits, real-time measurement by SV-Profiler at transducer depth were directly applied during acquisition with SIS Seafloor Information System.Data are unprocessed and can therefore contain incorrect depth measurements (artifacts) if not further processed. Note that refraction errors can be expected due to the lack of proper SVP.The data are archived at the Federal Maritime and Hydrographic Agency of Germany (Bundesamt für Seeschifffahrt und Hydrographie, BSH) and provided to PANGAEA database for data curation and publication. Ancillary sound velocity profiles (SVP) files from the cruise are archived at the BSH, thus SVP files are added to this dataset.Data acquisition and provision were accomplished within REEBUS project (Role of Eddies in the Carbon Pump of Eastern Boundary Upwelling Systems) as a supplement to benthic gear deployment and side scan sonar survey; It also contributes to DAM Underway Project.
description: These data should not be used for navigational purposes
DOI: 10.1594/pangaea.969557
title: Geochemical composition of the sedimentary record of Lake Zoñar (Spain)

description: High-resolution geochemical analysis of a 6-m-long sediment core from Zoñar Lake, southernSpain, provides a detailed characterisation of major changes in lake and watershed processes during the last 4,000 years. This dataset presents major, trace and earth rare elements. Major elements (Fe, Mn, Al, Ca, Mg and K) were quantified using a Perkin Elmer model 5100 Atomic Absorption Spectrometer, model 5100 ZLZEEMAN with an analytic error of 2%. Trace and REE (Li, Rb, Cs, Be, Sr, Ba, Sc, V, Cr, Co, Ni, Cu, Zn, Ga, Y, Nb, Ta, Zr, Hf, Mo, Sn, Tl, Pb, U, Th, La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb and Lu) were determined by Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) following HNO3+HF digestion. Measurements were made in triplicate by spectrometry (Perkin-Elmer Sciex Elan 5000) using Re and Rh as internal standards.
DOI: 10.1594/pangaea.971875
title: Dissolved neodymium isotopic composition, rare earth element and trace metal concentrations of surface water in the South Pacific Ocean from the SONNE cruise SO289 (GEOTRACES cruise GP21)

description: This dataset contains dissolved radiogenic neodymium (Nd) isotopes, rare earth element (REE) and trace metal (TM) concentrations of surface water in the South Pacific Ocean collected during the cross-Pacific GEOTRACES GP21 expedition (Chile-New Caledonia) with the German research vessel SONNE (SO289), which took place between February 23 and April 4, 2022. 20-40 L of surface seawater was collected either from the Niskin bottles attached to a stainless steel CTD rosette or from a trace-metal-clean underway tow-fish for Nd isotopes and REE concentrations. TM samples for dissolved manganese (dMn), dissolved iron (dFe), and dissolved aluminum (dAl) were collected from the tow-fish.Samples for Nd isotopes were pre-concentrated onboard by adsorption on Fe hydroxide precipitates and measured with a Neptune Plus Multicollector-Inductively Coupled Plasma Mass Spectrometer (MC-ICP-MS) after purification in the home laboratory. REE concentrations were pre-concentrated offline using a SeaFAST system and analyzed on a Thermo Element XR ICP-MS coupled with a CETAC "Aridus 2" desolvating nebulizer to reduce oxide formation. Dissolved Mn and Fe were pre-concentrated using SeaFast (SC-4 DX; ESI) and then measured on the same Thermo Element XR ICP-MS. Dissolved Al was analyzed shipboard using a Carey Eclipse fluorimeter. Phytoplankton pigment analysis (chlorophyll-a concentrations) were measured using a reverse-phase high-performance liquid chromatography (HPLC) (Dionex UltiMate 3000 LC system, Thermo Scientific).
DOI: 10.1594/pangaea.972064
title: Electromagnetic Induction (EMI) data from a GF Instruments CMD-Explorer of project KARST in Antalya Bay (Türkiye)

description: We conducted EMI measurements along the Konyaaltı Beach in Antalya (Tükiye) on the 6th of March 2023. The EMI survey simultaneously collected two different types of data at multiple depth levels. An electromagnetic signal, transmitted into the ground, returns two signals, the Quadrature data (linked to the apparent electrical conductivity) and the In Phase data which is proportional to apparent magnetic susceptibility. The measurements were carried out with the GF Instruments CMD-Explorer (dipole centre distance: 1.48 m, 2.82 m and 4.49 m). The measuring device was attached to the operator and measurements were performed at walking speed at 10 Hz sampling frequency (~15 cm spacing between measurements). We collected two parallel profiles along Konyaaltı Beach, which were measured with two constant distances to the waterline (~15 m and ~45 m distance from the waterline). Anthropogenic constructions such as beach pavilions seem to influence the measurements along the upper profile while the profile closer to the waterline appears error-free.
DOI: 10.1594/pangaea.972091
title: Tree-ring width measurements of Douglas fir from Bad Kissingen from 1979 to 2023

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972656
title: Tree-ring width measurements of Douglas fir from Bebenhausen from 1908 to 2017

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972657
title: Tree-ring width measurements of Douglas fir from Willer-sur-Thur from 1933 to 2023

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
description: Tree ring failures inserted in WILL0002 and WILL0014 in 1945, in WILL0002, WILL0003 and WILL0008 in 1947, each with value 3
DOI: 10.1594/pangaea.972658
title: Tree-ring width measurements of Douglas fir from Uffholtz from 1931 to 2023

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
description: Tree ring failure inserted in UFFH0012 in 2023 with value 3
DOI: 10.1594/pangaea.972659
title: Tree-ring width measurements of Douglas fir from St. Florian am Inn from 1984 to 2022

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972660
title: Tree-ring width measurements of Douglas fir from Staufen im Breisgau from 1960 to 2022

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
description: Tree ring failure inserted in STA20001 in 1990 with value 3
DOI: 10.1594/pangaea.972661
title: Tree-ring width measurements of Douglas fir from Staufen im Breisgau from 1944 to 2022

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972662
title: Tree-ring width measurements of Douglas fir from Rottenburg from 1979 to 2021

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972663
title: Tree-ring width measurements of Douglas fir from Ragow-Merz from 1940 to 2022

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972664
title: Tree-ring width measurements of Douglas fir from Thurnau from 1971 to 2021

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972665
title: Tree-ring width measurements of Douglas fir from Pielitz from 1951 to 2021

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
description: Tree ring failures inserted in PIEL0006 in 1962 and 1963 each with value 3
DOI: 10.1594/pangaea.972666
title: Tree-ring width measurements of Douglas fir from Rippenweier from 1927 to 2016

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972667
title: Tree-ring width measurements of Douglas fir from Thurnau from 1902 to 2021

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.
DOI: 10.1594/pangaea.972668
title: Tree-ring width measurements of Douglas fir from Rauen from 1936 to 2022

description: Wood samples from Douglas fir trees were taken using an increment borer. From each tree two opposing increment cores were taken at breast height. The sampled trees stood in an area of ~50x50 meters. Total ring width was measured and digitized. The resulting two radii measurements of each tree were visually synchronized and averaged to form a tree-ring series. Additionally, metadata were collected such as tree height, circumference and provenance (coastal, interior). The tree-ring data were used to investigate the resilience, resistance and recovery of the Douglas fir trees to severe drought events and to perform climate sensitivity analysis. This tree-ring dataset was part of a sampling campaign to assess the growth potential of Douglas fir trees until the year 2100. Annual tree growth variability until 2100 was modeled for Germany (including the river basins draining to Germany) with a spatial resolution of 12x12 km using regional climate projections ensemble.