cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.774780
title: (Table T1) Dissolved fluoride concentrations in pore waters of ODP Legs 204 and 201 sediments

description: Dissolved fluoride was determined for pore waters at eight sites drilled on Hydrate Ridge during Ocean Drilling Program (ODP) Leg 204 and one site drilled in the Peru Trench during ODP Leg 201. All nine sites contain a shallow (&lt;20 m) sulfate-methane transition (SMT) above abundant methane including gas hydrate. For Sites 1248, 1249, and 1250 on the crest of Hydrate Ridge, F- concentrations are significantly lower than that of seawater in the shallowest samples (&lt;50 µM), rise to a broad maximum, and generally decrease with depth. The low values at the top are consistent with rapid F- removal at or near the seafloor, and the relatively smooth F- profiles are consistent with high upward fluid fluxes. In contrast, Sites 1244, 1245, 1247, 1251, and 1252 from the flanks and slope basins of Hydrate Ridge and Site 1230 from the Peru Trench have F- profiles apparently characterized by two lows with an intervening high. Processes involving sediment components appear to consume F- at shallow depth, release F- at intermediate depth, and consume F- again at deeper depth. The upper low in F- concentrations consistently lies near the SMT where pore water alkalinity and Mg2+ profiles suggest precipitation of Mg-rich carbonate. A similar pattern occurs at other sites drilled into methane-charged sediment. We speculate that Mg-rich carbonates (e.g., high-Mg calcite, protodolomite, and dolomite) remove F- from pore water near the SMT but, with burial and recrystallization, return F- to pore waters at depth. Authigenic Mg-rich carbonates conceivably represent a major sink of F- from the ocean, although additional work is needed to confirm this idea.
description: Supplement to: Dickens, Gerald Roy; Donohue, Catherine M; Snyder, Glen T (2006): Dissolved fluoride concentrations in methane-charged sediment sequences. In: Tréhu, AM; Bohrmann, G; Torres, ME; Colwell, FS (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 204, 1-22
DOI: 10.1594/pangaea.484478
title: Hydrochemistry measured on water bottle samples at station SAVE3/116-1

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.728278
title: (Figure 8) Range chart of calcareous nannofossils in ODP Hole 116-719A

description: X = very rare (1-2 specimens), R = rare 3-5 specimens), F = few 6-20 specimens), C = common (20-100 specimens), A = abundant (&gt;100 specimens), W = very abundant &gt;80%), ? = questionable present, - = not present
DOI: 10.1594/pangaea.748236
title: Hydrography on standard level calculated from water bottle samples of RV Priliv in 1971
DOI: 10.15468/dl.xxpvzr
title: Occurrence Download

description: A dataset containing 5253 species occurrences available in GBIF matching the query:
{
 "TaxonKey" : [
 "is Roseodendron chryseum (S.F.Blake) Miranda"
 ]
}

 The dataset includes 5253 records from 55 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0031230-240626123714530/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.776048
title: (Table 2) Chemical composition of potassium feldspars from DSDP Hole 19-192A

description: Secondary potassium feldspar (K-feldspar) in oceanic basalts represented by low-temperature sanidine with low content of albite molecule. K-feldspar replaces nucleus of phenocrysts and large microlites of plagioclase. Occurrence of K-feldspar increases with age of rocks; in Pliocene and Pleistocene basalts from zones of mid-ocean ridges K-feldspar is absent. K-feldspar is developed in basalts of various geological, textural and structural types. Correlation of K-feldspar occurrence with primary alkalinity of basalts is absent. High (1-6%) contents of K2O in basalts in almost all cases are associated with development of K-feldspars in them. In basalts containing K-feldspars, a clear correlation between K2O and H2O (R = 0.55) is observed.
description: Supplement to: Simanovich, Igor M (1979): Potassium feldspar in oceanic basalts. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 14(1), 52-61
DOI: 10.1594/pangaea.858392
title: Time series of atmospheric water vapour at station MDO1_S1
DOI: 10.1594/pangaea.615294
title: Description of the soil of core LD98_t12

description: For the position of the transects t, v, and w see also figure 3-1
DOI: 10.1594/pangaea.730132
title: (Table 75) Chemical composition of &lt;0.002 mm grain size fraction from volcanoclastic sediments (intercalated with basalts) of the Nauru Basin at DSDP Site 61-462

description: Type II - semiordered alternation of smectite layers, according to J. Mering.
DOI: 10.1594/pangaea.787392
title: (Table T5) Geochemical composition of olivine from ODP Hole 176-735B

description: Number of ions is calculated on the basis of 4 oxygen atoms.
DOI: 10.1594/pangaea.615306
title: Description of the soil of core LD98_t3

description: For the position of the transects t, v, and w see also figure 3-1
DOI: 10.1594/pangaea.890690
title: X-ray fluorescence analyses of Branddam East Pan sediment sequence (ǁKaras Region, Namibia) by XRF PANalytical epsilon 3XL

description: X-ray fluorescence analyses have been done at sediment samples from a drill core at Branddam East Pan (Namibia) during the GeoArchives campaigns (Project Spaces).
DOI: 10.1594/pangaea.829341
title: Thermal conductivity of IODP Hole 340-U1398A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.676977
title: Ozone measurements from station Barrow (1993-04)
DOI: 10.1594/pangaea.681228
title: Meteorological synoptical observations from station Ny-Ålesund (2002-12)

description: On 2016-07-06 some corrections on the wind speed were made for this dataset. The old version is available at: ftp://ftp.bsrn.awi.de/nya/OldVersions_2016-07-06_oldSYNOPS/
DOI: 10.1594/pangaea.720881
title: Documentation of sediment core GIK23454-1
DOI: 10.1594/pangaea.789160
title: (Table 4) Inorganic and organic geochemistry of postcruise samples at DSDP Hole 93-603B
DOI: 10.1594/pangaea.670133
title: Physical oceanography of CTD station T75 off Ancon, 2002, Peru
DOI: 10.1594/pangaea.829264
title: P-Wave velocity (PWC) from IODP Hole 340-U1400B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.674432
title: Radiosonde measurements from Neumayer Station (1998-12)
DOI: 10.1594/pangaea.747953
title: Meteorological observations during CORTGENE cruise from Rotterdam to Batavia started at 1853-08-10
DOI: 10.1594/pangaea.720174
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 66-490

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: 10.5281/zenodo.10183718
title: Anonymized weights
DOI: 10.1594/pangaea.720185
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 67-497

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.829320
title: Magnetic remanence from IODP Hole 340-U1397B

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.807084
title: (Table 3) Geochemistry of clinopyroxene at DSDP Leg 81 Holes

description: Concentrations lower than 0.3% are not considered representative.
DOI: 10.1594/pangaea.823996
title: P-Wave velocity (PWB) from IODP Hole 320-U1335A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.890694
title: X-ray fluorescence analyses of Witpan sediment sequence (Northern Cape, South Africa) by XRF PANalytical epsilon 3XL

description: X-ray fluorescence analyses have been done at sediment samples from a drill core and a pit at Witpan (South Africa) during the GeoArchives campaigns (Project Spaces).
DOI: 10.1594/pangaea.667372
title: (Table 3) Isotope ratios of smectites from DSDP Hole 52-418A
DOI: 10.1594/pangaea.825949
title: (Table S19) U-channel paleomagnetic data of IODP Hole 320-U1333C
DOI: 10.1594/pangaea.828828
title: Gas measurements from IODP Hole 339-U1388A

description: Geocode = Top depth CSF-A (m)
DOI: 10.1594/pangaea.750605
title: Meteorological observations during Margaretha en Maria cruise from Bremen to New York started at 1852-05-22
DOI: 10.1594/pangaea.849444
title: Ground-penetrating radar (GPR) point measurements of ice thickness on Griesskogelferner in 2008
DOI: 10.1594/pangaea.816414
title: (Table 10) Geochemistry of bulk rock at DSDP Hole 69-504B
DOI: 10.1594/pangaea.718834
title: Ultra-violet measurements from station Sioux Falls (2009-04)

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 2017-02-03.
DOI: 10.1594/pangaea.763304
title: Table 1: U-Pb analyses of zircons and monazites of paragneisses which belong to the high grade metamorphic basement of Wilson Terrane

description: Samples of high grade metamorphic basement rocks of Wilson Terrane cropping out in the Deep Freeze Range and on Kay Island were collected during GANOVEX VI to study their isotopic evolution. The age and origin of granulite facies gneisses and of their migmatite host rocks are especially of interest for the interpretation of the geological and tectonic development of North Victoria Land. Another important research aspect is the influence of the polyphase metamorphic evolution on the isotopic systems of whole rocks and minerals like zircon, garnet, orthopyroxene, amphibole and feldspar.
description: Zircon ages vary between 480 Ma and 488 Ma, monazites yield ages between 482 Ma and 485 Ma. In Table 1 ages are calculated from Ma to ka.
description: Supplement to: Klee, Susanne; Baumann, Albrecht; Thiedig, Friedhelm (1992): 9. Age relations of the high grade metamorphic rocks in the Terra Nova Bay Area, North Victoria Land, Antarctica: a preliminary report. Polarforschung, 60(2), 101-106
DOI: 10.1594/pangaea.829048
title: Magnetic remanence from IODP Hole 339-U1391A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.869062
title: Documentation of sediment core GIK18402-3
DOI: 10.1594/pangaea.723365
title: Description of profile 7441-108
DOI: 10.1594/pangaea.861366
title: Impact of CO2 enrichment on organic matter dynamics - Enrichment experiment

description: Cells were incubated for 3 days at in-situ temperature and in the dark. Incubations were analysed for bacterial abundances by flow cytometry after nucleic acid staining with Sybr Green I (Invitrogen). For determination of LAP activities, L-leucyl-4-methylcoumarinyl-7-amide was added to final concentrations of 50 µmo/L. The initial abundance of free-living bacteria was 2.0 x 10**5 cells/ml, representing about 20% of the total bacterioplankton community.
DOI: 10.1594/pangaea.664247
title: Oceanography at CTD/bottle station IFREMER_1088
DOI: 10.1594/pangaea.748146
title: Hydrography on standard level calculated from water bottle samples of RV Lyra in 1967
DOI: 10.1594/pangaea.733285
title: Physical oceanography during Moana Wave cruise HOT-22 on section PRS2
DOI: 10.1594/pangaea.695370
title: (Table 1) Strontium isotope ratios of planktonic foraminifera and ostracoda from ODP Hole 120-748B on the Kerguelen Plateau, Indian Ocean

description: Stable and radiogenic isotopic and sedimentological data from sub-Antarctic deep sea sediment cores reveal a temporal link between changes in seawater 87Sr/86Sr ratios and major episodes of late Eocene-early Oligocene climate change. The 87Sr/86Sr records show two major inflections, one at 38-39 Ma near the middle/late Eocene boundary, followed by another at 33.4 Ma. Similarly, the oxygen isotope, ice-rafted debris, and clay assemblage records indicate two important climatic events: the appearance of alpine glaciers and/or small ice-sheets on Antarctica in the late Eocene at 38-39 Ma, followed by a rapid transition to larger and more permanent temperate ice-sheets in the early Oligocene at 33.4 Ma. Moreover, during the early Oligocene 30-33 Ma. three to four inferred peaks in glacial activity appear to coincide with subtle steps in the 87Sr/86Sr record. The coupled variations in climate and seawater Sr isotope ratios during the Eocene/Oligocene imply a strong causal link between the two. Either changes in climate directly influenced patterns of continental weathering and hence seawater chemistry, and/or a tectonic event e.g., uplift.as reflected in weathering and seawater chemistry triggered relatively abrupt changes in global climate.
description: Supplement to: Zachos, James C; Opdyke, Bradley N; Quinn, Terrence Michael; Jones, Charles E; Halliday, Alex N (1999): Early cenozoic glaciation, antarctic weathering, and seawater 87Sr/86Sr: is there a link? Chemical Geology, 161(1-3), 165-180
DOI: 10.1594/pangaea.711223
title: (Table 3) Phase distribution of elements from ODP Hole 107-650A

description: Phase: 1 = exchangeable adsorbed elements, carbonates, and carbonate bound elements. 2 = easily reducible fraction (including Mn-oxides and co-precipitated elements). 3 = oxidizeable phases, organic matter, and sulphides. 4 = residual.
DOI: 10.1594/pangaea.509877
title: Total organic carbon, nitrogen and phosphorus oxygen content of sediment core GIK01152, Arabian Sea, African continental margin (Appendix)
DOI: 10.1594/pangaea.713306
title: (Table DR1) Silicic tephras in ODP Hole 162-985B
DOI: 10.1594/pangaea.829321
title: Magnetic remanence from IODP Hole 340-U1398A

description: Geocode = Depth CSF-A (m)
DOI: 10.1594/pangaea.712418
title: Fluorine and chlorine concentrations and Cl isotope ratios of serpentines of ODP Site 195-1200

description: Chlorine stable isotopes (delta37Cl) and halogen concentrations (e.g. Br/Cl) in 168 pore Fluids and 23 serpentines and other solids from three subduction zones, the Nankai Trough, Costa Rica, and Mariana Forearc, provide critical information on fluid sources, flow paths, and reaction conditions. The delta37Cl values of pore fluids at the Nankai and Costa Rica subduction zones, are significantly more negative (minimum -7.8‰, 2 sigma +/- 0.3‰) than seawater value (0‰). At Nankai Trough, the minimum delta37Cl value is situated below the décollement and evolves laterally from -7.8‰ at the most arcward ODP Site 808, to -7.1‰ at Site 1174, not, vert, similar 2 km seaward from Site 808, and to -5.8‰ at the reference Site 1173. At Costa Rica, along the décollement the minimum delta37Cl value evolves from -5.5‰ at the most arcward ODP Site 1040/1254, to -3.2‰ at Site 1043/1255, ~1 km seaward, and to 0‰ at the reference Site 1039/1253. At both subduction zones, the Br/Cl ratios are higher than the seawater value (1.5 * 10**-3) and also show seaward evolutions. These pore fluids originate from greater depth arcward, at &gt;= 250 °C, from hydrous mineral formation that preferentially incorporates 37Cl and excludes Br. In contrast, the delta37Cl values in the pore fluids at the Mariana serpentine mud volcanoes are higher than the seawater value (+ 0.3‰ to + 1.8‰); and the Br/Cl ratios are lower. These pore fluid values and the high Cl concentrations with positive delta37Cl values (+ 1.2 to + 6.0‰) in the serpentines, support that the upwelling pore fluid originates from dehydration of the subducting slab that releases water enriched in 37Cl, into the fluid phase.The constancy of the ocean delta37Cl over the past 200 Ma suggests that the isotopically fractionated chlorine in serpentinites and the Cl exchanged in subduction zones are efficiently recycled back into seawater. If the efficiency is &lt; 100%, the residual would be transferred to the mantle, with a maximum Cl flux between 2 to 3 * 10**17 moles/Ma that would lead to an isotopic difference between the mantle and seawater over the age of the earth on the order of a few per mil.
description: Supplement to: Wei, Chih-Lin; Kastner, Miriam; Spivack, Arthur J (2008): Chlorine stable isotopes and halogen concentrations in convergent margins with implications for the Cl isotopes cycle in the ocean. Earth and Planetary Science Letters, 266(1-2), 90-104
DOI: 10.1594/pangaea.720190
title: (Table Raw) Point-count data and petrological parameters of sands/sandstones from DSDP Site 67-499

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.773879
title: Summarized lithologic description from IODP Hole 316-C0007A

description: Geocode = [m, CMP] Top Depth DSF, MSF, WSF and CSF-B
DOI: 10.1594/pangaea.615289
title: Description of the soil of core LD98_t10a

description: For the position of the transects t, v, and w see also figure 3-1
DOI: 10.1594/pangaea.859820
title: Surface microlayer data during KOSMOS 2011 mesocosm experiment in the Raunefjord