cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.720134
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 15-148

description: Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline quartzP = Plagioclase feldsparK = Potassium feldsparLvo = Other volcanic lithicLvd = Devitrified vitric volcanic lithicLvv = Vitric volcanic lithicLvf = Volcanic lithic with felsitic textureLvmi = Volcanic lithic with microlitic textureLvl = Volcanic lithic with lathwork textureLvp = Pyroclastic volcanic lithicLmv = Metavolcanic lithicLmm = Polycrystalline mica lithicLmt = Quartz-mica tectonite lithicLma = Quartz-feldspar-mica aggregate lithicLmp = Phyllite lithicLsa = Argillite-shale lithicLsc = Sedimentary carbonate lithicLsch = sedimentary chert or cherty argillite lithicLsi = Siltstone sedimentary lithicM = Phyllosilicate mineralsD = Dense mineralsCarb = Carbonate mineralsBio = Bioclastic debris (siliceous and/or carbonate)Misc = Miscellaneous and unidentifiedQ = Total quartzose grainsL = Unstable lithic grainsLm = Metamorphic lithic grainsLv = Volcanic-hypabyssal (and volcaniclastic) lithic grainsLs = Sedimentary lithic grainsLvm = Volcanic-hypabyssal and metavolcanic lithic grainsLsm = Sedimentary and metasedimentary lithic grainsLst = Sedimentary and polycrystalline quartz grainsF = Total feldspar grainsQp = Polycrystalline quartz grainsQ = Qm + Qpw + QptQp = Qpw + QptL = Lm + Lv + LsLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpLm = Lmv + Lmm + Lmt + LmaLsm = Ls + Lmm + Lmt + LmaLvc = Lvf + Lvmi + LvlLv = Lvo + Lvv + Lvf + Lvmi + Lvl + LvpF = P + KLs = Lsa + LscLvm = Lv + LmvLst = Ls + QpQFL%Q = 100Q/(Q + F + L)QFL%F = 100F/(Q + F + L)QFL%L = 100L/(Q + F + L)QmKP%Qm = 100Qm/(Qm + P + K)QmKP%P = 100P/(Qm + P + K)QmKP%K = 100K/(Qm + P + K)LvfLvmiLvl%Lvf = 100Lvf/LvcLvfLvmiLvl%Lvmi = 100Lmi/LvcLmLvLs%Lm = 100Lm/LLmLvLs%Lv = 100Lv/LLmLvLs%Ls = 100Ls/LQpLvmLsm%Qp = 100Qp/(L + Qp)QpLvmLsm%Lvm = 100Lvm/(L + Qp)QpLvmLsm%Lsm = 100Lsm/(L + Qp)LvfLvmiLvl%Lvl = 100Lvl/Lvc
DOI: 10.1594/pangaea.723323
title: Description of profile 7140-307
DOI: 10.1594/pangaea.824532
title: Carbonate analysis from IODP Hole 318-U1359C

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.910683
title: (Table S16) Ichthyolith abundance in IODP Site 342-U1406

description: Ichthyolith counts (&gt;38µm) and calculated ichthyolith accumulation rates determined in this study. Revised CCSF-A Depth Scale from: van Peer et al. 2017. Sediment dry bulk density was obtained from shipboard data (available from LIMS database) http://web.iodp.tamu.edu/LORE/?appl=LORE&reportName=mad&action=show&filters=[%22x_expedition%20in%20(%27342%27)%22,%22x_site%20in%20(%27U1406%27)%22].Ages based on shipboard magnetostratigraphy, see table S17 (this study, doi:10.1594/PANGAEA.910684) for more details.
DOI: 10.1594/pangaea.808023
title: (Figure 8) Radiolarian range chart of ODP Site 138-851, part I

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.828729
title: P-Wave velocity (PWC) from IODP Hole 336-U1382A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.723363
title: Description of profile 7441-106
DOI: 10.1594/pangaea.677012
title: Ozone measurements from station Barrow (1997-07)
DOI: 10.1594/pangaea.701712
title: (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 39-3551 in the South Atlantic Ocean

description: Mid-Late Campanian
DOI: 10.1594/pangaea.707686
title: (Table 1) B content, d11B, δ¹⁸O, degree of alteration, and lithology of basalts from ODP Hole 504B

description: Boron contents and boron isotopic compositions were determined for the uppermost 1.3 km section of typical 6.2 Ma oceanic crust from DSDP/ODP Hole 504B, Costa Rica Rift, Galapagos Spreading Center. Both the boron content and the d11B value in the oceanic crust are controlled by two types of alteration: 1. (1) low-temperature alteration (0 to 60°C; Zones I and II) and2. (2) high-temperature hydrothermal alteration (200 to 400°C; Zones III and IV).Basalts subjected to the low-temperature alteration are characterized by their relatively high boron contents (0.69 to 19.3 ppm) and high d11B values (+2.2 to +10.6‰), indicating uptake of boron into secondary phases in equilibrium with seawater or evolved seawater. Hydrothermally altered basalts contain less abundant boron (0.17 to 0.52 ppm) and relatively constant d11B values (?0.1 to +1.0‰). Although basalts from the upper part of these hydrothermal zones (&lt;1300 mbsf) show equilibrated boron content and d11B value with aqueous fluid, effective leaching of boron from basalt is predominant in the lower part (&gt;1300 mbsf). Original boron content and d11B value of the Hole 504B MORB were 0.35 ppm and +0.2‰, respectively. The present data provide fundamental information in understanding of the distribution of boron and boron isotopes in the oceanic crust.
DOI: 10.1594/pangaea.828546
title: P-Wave velocity (PWL) from IODP Hole 323-U1341B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.872602
title: Meteorological measurements in Up Park Camp, Jamaica from February 1853- January 1854, digitized version

description: The records were taken two times a Day at 9:30 and 15:30. In 1852 the Royal Engineers (British Army) under the supervision of Colonel Sir Henry James started a network of meteorological observations in the principal foreign stations. Sir James born in 1803 in Rose Vale (Cornwall, UK) study at the Royal Military Academy (Woolwich) and he commissioned the 22 September 1826 in the Royal Engineers. He was promoted to Capitan in 1846 and to Colonel in 1857. From 1854 he was Director-General of the Ordnance Survey (the national mapping agency of Great Britain). He collaborates in the invention of the photozincography (1860) and used this method to preserve historic manuscripts. He retired in 1875 and died on 14 June 1877 in Southampton. The stations were supplied with meteorological instruments and a book entitled ""Instructions for taking Meteorological Observations"" (James, 1851) revised in 1861 (James, 1861). So, the Royal Engineers start to take homogenous meteorological measurements (same instruments, same observational methodology) all around the world. The observations were taken twice a Day (at 9.30h and 15.30h), for the barometer, the dry and wet bulb thermometer, wind (direction and force), amount of cloud, together with the computed values of the dew point, vapour tension, and relative humidity. Also give daily record of maximum temperature in the sun, maximum temperature in the shade, maximum temperature of evaporation, minimum temperature in the shade, minimum temperature on the grass, minimum temperature of evaporation, rainfall in past 24 hours on the ground, rainfall in past 24 hours at 20 feet above the ground, maximum pressure of wind in past 24 hours, amount of ozone, and Remarks (state of the sky, prevalent diseases, arrival of birds of passage, leafing of trees). In addition hourly readings of the instruments were taken on 21st March, 21st June, 21st September, and 21st December and at certain stations readings were taken all the 21st. Unfortunately not all the variables were taken in all stations, for this we explain in each location the retrieved observations. James H 1851. Instructions for taking Meteorological Observations at the Principal Foreign Stations of the Royal Engineers. London: HMSO./ James H 1861. Instructions for taking Meteorological Observations with tables for their correction, and notes on meteorological phenomena. London: George E Eyre and William Spottiswoode.---The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480
DOI: 10.1594/pangaea.789220
title: (Table 1) Sediment descriptions, stage, calcium carbonate, organic carbon and delta 13C at DSDP Hole 93-603B
DOI: 10.1594/pangaea.829278
title: P-Wave velocity (PWL) from IODP Hole 340-U1397A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.805169
title: (Table 4) Sr, Nd, Pb, and O isotope ratios and isotope dilution-determined trace element concentrations in ODP Site 136-843 basalts

description: O analyses performed at the University of Minnesota. All other analyses performed at the University of Hawaii (UH). O isotope ratios are normalized to SLAP (d18O VSMOW = -55.0 per mil) and reported relative to VSMOW. The d18O value for NBS-28 quartz on this scale is +9.5 ± 0.15 per mil. Isotopic fractionation correction for Nd is 148NdO/144NdO = 0.242436 (148Nd/144Nd = 0.241572); for Sr it is 8 6Sr/88Sr = 0.1194. Pb values are adjusted relative to the NBS 981 values of Todt et al. (1984). Nd isotopic data are reported relative to UH measured 143Nd/144Nd values for the La Jolla Nd standard of 0.511855 ± 0.000012 total range.Sr isotopic data are reported relative to UH measured 87Sr/86Sr values for NBS 987 of 0.71025 ± 0.00002 total range. Within-run uncertainties on sample Nd and Sr isotopic ratios are less than total ranges measured on La Jolla Nd and NBS 987 standards. Estimated uncertainty on 206Pb/204Pb is ± 0.010; on 207Pb/204Pb it is ± 0.009; and on 208Pb/204Pb it is ± 0.032; based on total ranges measured for NBS 981. Total blanks are: Pb = 5-40 pg, Nd &lt; 20 pg, and Sr &lt; 120 pg.
DOI: 10.1594/pangaea.747903
title: Meteorological observations during CHINA cruise from Soerabaija to Nieuwediep started at 1854-01-07
DOI: 10.1594/pangaea.674596
title: Radiosonde measurements from station Kwajalein (1999-02)
DOI: 10.1594/pangaea.746533
title: Meteorological observations during DELPHINA cruise from Texel to Kaap de Goede Hoop started at 1821-04-20
DOI: 10.1594/pangaea.826465
title: Pass-through measurements of magnetic susceptibility from IODP Hole 329-U1367E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.875811
title: Meteorological synoptical observations from station Lindenberg (2011-02)
DOI: 10.1594/pangaea.757547
title: Radiosonde measurements from station Ny-Ålesund (2010-11)

description: The Ny-Ålesund radiosonde program is part of the GCOS Reference Upper-Air Network (GRUAN). Please consider using the Ny-Alesund reference radiosonde data with higher temporal resolution and uncertainty values for all height levels, available via http://www.gruan.org.
DOI: 10.1594/pangaea.712592
title: (Table 2) Sr isotope ratios of planktonic foraminifera from DSDP Hole 72-516
DOI: 10.1594/pangaea.720795
title: Documentation of sediment core GIK23259-3
DOI: 10.1594/pangaea.721001
title: Isotope ratios of sediments from DSDP Hole 47-397 (Table 1)

description: We report the Sr, Nd and Pb isotopic compositions (1) of 66 lava flows and dikes spanning the circa 15 Myr subaerial volcanic history of Gran Canaria and (2) of five Miocene through Cretaceous sediment samples from DSDP site 397, located 100 km south of Gran Canaria. The isotope ratios of the Gran Canaria samples vary for 87Sr/86Sr: 0.70302-0.70346, for 143Nd/144Nd: 0.51275-0.51298, and for 206Pb/204Pb: 18.76-20.01. The Miocene and the Pliocene-Recent volcanics form distinct trends on isotope correlation diagrams. The most SiO2-undersaturated volcanics from each group have the least radiogenic Sr and most radiogenic Pb, whereas evolved volcanics from each group have the most radiogenic Sr and least radiogenic Pb. In the Pliocene-Recent group, the most undersaturated basalts also have the most radiogenic Nd, and the evolved volcanics have the least radiogenic Nd. The most SiO2-saturated basalts have intermediate compositions within each age group. Although the two age groups have overlapping Sr and Nd isotope ratios, the Pliocene-Recent volcanics have less radiogenic Pb than the Miocene volcanics.At least four components are required to explain the isotope systematics of Gran Canaria by mixing. There is no evidence for crustal contamination in any of the volcanics. The most undersaturated Miocene volcanics fall within the field for the two youngest and westernmost Canary Islands in all isotope correlation diagrams and thus appear to have the most plume-like (high 238U/204Pb) HIMU-like composition. During the Pliocene-Recent epochs, the plume was located to the west of Gran Canaria. The isotopic composition of the most undersaturated Pliocene-Recent volcanics may reflect entrainment of asthenospheric material (with a depleted mantle (DM)-like composition), as plume material was transported through the upper asthenosphere to the base of the lithosphere beneath Gran Canaria. The shift in isotopic composition with increasing SiO2-saturation in the basalts and degree of differentiation for all volcanics is interpreted to reflect assimilation of enriched mantle (EM1 and EM2) in the lithosphere beneath Gran Canaria. This enriched mantle may have been derived from the continental lithospheric mantle beneath the West African Craton by thermal erosion or delamination during rifting of Pangaea. This study suggests that the enriched mantle components (EM1 and EM2) may be stored in the shallow mantle, whereas the HIMU component may have a deeper origin.
description: Supplement to: Hoernle, Kaj; Tilton, George; Schmincke, Hans-Ulrich (1991): Sr-Nd-Pb isotopic evolution of Gran Canaria: evidence for shallow enriched mantle beneath the Canary Islands. Earth and Planetary Science Letters, 106(1-4), 44-63
DOI: 10.1594/pangaea.730324
title: Documentation of sediment core GIK23462-2
DOI: 10.1594/pangaea.751885
title: Meteorological observations during San Jose cruise from Montevideo to Cádiz started at 1778-04-21
DOI: 10.1594/pangaea.751769
title: Meteorological observations during Rhoon en Pendrecht cruise from Rotterdam to Batavia started at 1836-04-25
DOI: 10.1594/pangaea.762623
title: Core-section summary for Hole 325-M0040A
DOI: 10.1594/pangaea.701486
title: Water temperature profiles from 20 XBT drops along the track of POSEIDON cruise POS231/1
DOI: 10.1594/pangaea.744748
title: Composition of subalkali basalts from the Jan Mayen Fracture Zone, Jan Mayen Ridge, and alkali rocks from the Southern Seamount in the Greenland Sea
DOI: 10.1594/pangaea.772101
title: CNS-analysis from IODP Hole 315-C0001F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.730166
title: (Table 25) Abundance of trace elements in basalts from the Gulf of California, DSDP Hole 65-485A
DOI: 10.1594/pangaea.817303
title: (Table 1 - part 1) Coarse silt (0.1-0.05 mm) fraction mineralogy at DSDP Leg 67 Holes: Heavy fraction

description: Sediment depth is given in mbsf. #1 = moderate.
DOI: 10.1594/pangaea.728318
title: (Table 1) Diatom species composition and distribution at ODP Site 116-717C

description: Autochthonous marine pelagic and allochthonous coastal and freshwater diatoms were encountered in five samples from the Ocean Drilling Program (ODP) Leg 116 Holes 717A, 717B, and 717C. Allochthonous diatoms were transported to the equatorial Indian Ocean from inland locations and coastal waters, respectively. The pelagic diatom assemblage consists mainly of warm and/or tropical diatoms known from the Neogene to Holocene. A stratigraphic marker, Rhizosolenia praebergonii var. robusta, which indicates Pliocene-Pleistocene (2.4-1.55 Ma) age of the sediments, was present in the samples from Core 116-717C-27X. Species composition of the whole assemblage is most similar to the tropical Indian Ocean Diatom Zone 6 of Schrader and supports an estimated age of 1.8-2.1 Ma for the sediments.
description: X = present, - = absent
description: Supplement to: Kaczmarska, Irena (1990): Diatoms at Site 717, Leg 116. In: Cochran, JR; Stow, DAV, et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 116, 239-242
DOI: 10.1594/pangaea.759922
title: Vitrinite reflectance and carbon chemistry of ODP Leg 122 samples (Table 1)

description: A summary of shipboard Rock-Eval measurements shows that organic matter in Upper Triassic siltstone from the Wombat Plateau is dominated by Type III kerogen and is thermally immature. Neocomian siltstone from the Exmouth Plateau similarly contain thermally immature Type III organic matter. Overlying Upper Cretaceous to Quaternary carbonates are poor in organic matter at both locations, yet significant amounts of methane-dominated gas are dissolved in the pore waters of the thick carbonate sequence present on the Exmouth Plateau. This dry gas is believed to have migrated from deeper and more mature strata containing Type III kerogen.
description: Sediment depth is given in mbsf. Vitrinite reflectance measurements (%Ro) made by W. Kalkreuth at the Geological Survey of Canada.
description: Supplement to: Snowdon, Lloyd R; Meyers, Philip A (1992): Source and maturity of organic matter in sediments and rocks from Sites 759, 760, 761, and 764 (Wombat Plateau) and Sites 762 and 763 (Exmouth Plateau). In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 309-315
DOI: 10.1594/pangaea.784899
title: Thermal conductivity of IODP Hole 333-C0011D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.775810
title: (Table T1) Chemical composition of celadonitic phyllosilicates from ODP Holes 206-1256C and 206-1256D

description: Sediment depth is given in mbsf. Chemical formulas were calculated for phyllosilicates based on a layer charge of 22 (10 oxygens and 2 hydroxyls).
DOI: 10.1594/pangaea.785305
title: Comparison of Sr isotope ratios of ODP Hole 131-808C

description: Pore fluid and sediment chemical and isotopic data were obtained at ODP Site 808, western Nankai trough, Japan. The isotopic data reported here (Tables 1, 2, 3, 4) were carried out in our shore-based laboratories to complement the shipboard inorganic geochemical data published in Shipboard Scientific Party (1991). The data include: hydrogen, oxygen, and strontium isotopic compositions of the pore fluids, carbon and oxygen isotopic compositions of biogenic and authigenic calcites, and preliminary mineralogical compositions of the authigenic precipitates in veins and in tubular-cylindrical structures, observed in the sediments between 870 and 1080 mbsf. These data do not support active pervasive fluid flow at the décollement zone nor at the frontal thrust. They do, however, support pervasive active lateral fluid flow above and particularly below the décollement.
description: Sediment depth is given in mbsf. For Sr-data of pore fluid ans stable iostope ratios see Kastner et al. 1993, datasets doi:10.1594/PANGAEA.785296.
description: Supplement to: Kastner, Miriam; Elderfield, Henry (1993): Data report: Compositions of fluids and authigenic phases in sediments of the Nankai Trough accretionary complex. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 423-425
DOI: 10.1594/pangaea.723367
title: Description of profile 7441-110
DOI: 10.1594/pangaea.826392
title: Reflectance spectroscopy and colorimetry from IODP Hole 329-U1366C

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.758302
title: Meteorological data from Jubany Station, King George Island, Western Antarctic Peninsula, 1999
DOI: 10.1594/pangaea.823469
title: (Table 4) Bulk geochemistry at DSDP Hole 54-424A recalculated on CaO-free basis
DOI: 10.1594/pangaea.891267
title: Radiolarian abundances from IODP Hole 349-U1431D
DOI: 10.1594/pangaea.776884
title: Description and distribution of lithologic units (VCD) from IODP Hole 331-C0017A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.885774
title: Meteorological observations at Laguna La Conceja (Ruidera, Spain) during 2009
DOI: 10.1594/pangaea.824841
title: Point measurements of magnetic susceptibility from IODP Hole 334-U1378B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.776368
title: Headspace-gas measurements from IODP Hole 331-C0013F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.713296
title: (Table 4) Oxygen isotopic composition and calculated equilibrium temperatures of formation for quartz from the transition zone and dike section of DSDP Hole 504B

description: Depth, sediment (m) is the sub-basement depth (m)
DOI: 10.1594/pangaea.723368
title: Description of profile 7441-111
DOI: 10.1594/pangaea.756079
title: (Table 15) Occurrence of calcareous nannofossils observed in the Oligocene samples from ODP Hole 115-714A

description: Specimens not identifiable to known species are excluded. Distribution chart: Numbers = calculated percentage in the indigenous flora, figures below the decimals are omitted; F = few (&gt;0.1% and &lt; 1% of indigenous forms); R = rare (&lt;0.1% of indigenous forms); c = common reworked occurrence (&gt; 1% and &lt; 10% of the total flora), f = few reworked occurrence (&gt;0.1% and &lt; 1% of the total flora); r = rare reworked occurrence (&lt;0.1% of the total flora), - = not present.
DOI: 10.1594/pangaea.826103
title: P-Wave velocity (PWL) from IODP Hole 327-U1363F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.826030
title: Interstitial water analysis from IODP Hole 327-U1363B

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.704814
title: (Table 1) Chemical composition of green clays in sandstone from different depths at ODP Site 126-793B

description: Microbial green marine clays in deep-sea sediments were recovered from the Izu-Bonin fore-arc basin at Leg 126 of the Ocean Drilling Program (ODP) along the Bonin-Mariana trench. Green spherical materials and remnants of dead microbial cells of filamentous bacteria are abundant in the green marine clays. Organic carbon and graphite were found in the volcanic sandstone. Transmission electron microscope observations clearly show processes of graphite mineralization from low-crystallinity to well-crystallized graphite. However, X-ray photoelectron spectrochemical analyses (micro-ESCA) indicate that the green marine clays contain high C (1s) of microbial origin carbon, and COO, C---O, C---C and graphite structures. Fourier transform infrared spectra (FT-IR spectra) of the green spherules show peaks between glauconite and celadonite. X-ray powder diffraction data show the presence of smectite and 1.03-1.22-nm mica-clay minerals with abundant zeolites, which are hydrothermal alteration products. The results suggest that fossil remnants of graphite mineralized organisms, in particular filamentous bacteria, might play an important role in the formation of green marine clays.
description: Supplement to: Tazaki, Kazue; Fyfe, William S (1992): Microbial green marine clay from Izu-Bonin (west Pacific) deep-sea sediments. Chemical Geology, 102(1-4), 105-118
DOI: 10.1594/pangaea.826094
title: Downhole temperature measurement from IODP Hole 327-U1363F

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.828430
title: Gamma ray attenuation bulk density from IODP Hole 323-U1343E

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.650351
title: Description of lithologic section units of Hole 310-M0009D

description: Abbreviations: encr=enrcusting, br=braching, rob=robust, tab=tabular, fol=foliaceous, mas=massive, frags/frag=fragments/fragmented, unident=unidentifies, CAB=coral-algal bindstone, ECR=encrustation, MB=microbiolite, HAL=Halimeda, IS=in situ, UK=unknown, gp=group; DEPTH applies to top depth of section unit
DOI: 10.1594/pangaea.750123
title: Meteorological observations during La Diana cruise from Montevideo to La Coruña started at 1776-01-16