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  • 1
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    (Table 1) Environmental and bulk geochmical data of soils, river SPM, and marine surface sediments (2017)
    PANGAEA
    Details
    Publication Date: 2023-03-14
    Keywords: Ain_AW1; Ain, France, Europe; Carbon, organic, total; Date/Time of event; Delta du Rhone; DEPTH, sediment/rock; DEPTH, soil; DEPTH, water; Doubs_DW1; Doubs, France, Europe; Durance_Du2; Durance, France, Europe; Elevation of event; Event label; Isere_IW1; Isere, France, Europe; Latitude of event; Location of event; Longitude of event; Lower Rhone, France, Europe; MUC; MultiCorer; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; pH; Precipitation, annual mean; Rhone_delta_A; Rhone_delta_AK45; Rhone_delta_B; Rhone_delta_C; Rhone_delta_D; Rhone_delta_K; Rhone_delta_L; Rhone_delta_N; Rhone_RW1; Rhone_RW10; Rhone_RW11; Rhone_RW12; Rhone_RW13; Rhone_RW2; Rhone_RW3; Rhone_RW4; Rhone_RW5; Rhone_RW6; Rhone_RW7; Rhone_RW8; Rhone_RW9; RhoS-1; RhoS-10; RhoS-11; RhoS-12; RhoS-13; RhoS-14; RhoS-15-1; RhoS-15-2; RhoS-16; RhoS-17; RhoS-18; RhoS-2; RhoS-20; RhoS-21; RhoS-22-1; RhoS-22-2; RhoS-23; RhoS-24; RhoS-25; RhoS-26; RhoS-27; RhoS-28; RhoS-29-2; RhoS-3; RhoS-30; RhoS-31; RhoS-32; RhoS-33; RhoS-34; RhoS-35; RhoS-36; RhoS-37; RhoS-38; RhoS-39-1; RhoS-4; RhoS-40; RhoS-41; RhoS-42; RhoS-44; RhoS-45; RhoS-46; RhoS-47; RhoS-48; RhoS-49; RhoS-5; RhoS-50; RhoS-6; RhoS-7; RhoS-8; RhoS-9; RHS12-10; RHS12-11; RHS12-12; RHS12-13; RHS12-14; RHS12-15; RHS12-16; RHS12-17; RHS12-18; RHS12-19; RHS12-2; RHS12-20; RHS12-21; RHS12-23-b; RHS12-3; RHS12-5; RHS12-6; RHS12-7; RHS12-8; RHS12-9; Saone_SW1; Saone_SW2; Saone_SW3; Saone_SW4; Saone, France, Europe; SOIL; Soil profile; Suspended particulate matter; Temperature, air, annual mean; Upper Rhone, France, Europe; Upper Rhone, Switzerland, Europe; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 372 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 2
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    Tracing tetraether lipids in the Rhône River system (2017)
    PANGAEA
    In:  Supplement to: Kim, Jung-Hyun; Ludwig, Wolfgang; Buscail, Rosalyne; Dorhout, Denise J C; Sinninghe Damsté, Jaap S (2015): Tracing tetraether lipids from source to sink in the Rhône River system (NW Mediterranean). Frontiers in Earth Science, 3, https://doi.org/10.3389/feart.2015.00022
    Details
    Publication Date: 2023-01-13
    Description: In this study, we investigated soils and river suspended particulate matter (SPM) collected in the Rhône and its tributary basins as well as marine surface sediments taken in the Rhône prodelta (Gulf of Lions, NW Mediterranean). Thereby, we traced the signal of branched glycerol dialkyl glycerol tetraethers (brGDGTs) from the source to sink via the Rhône River and its tributaries and identified sources of brGDGTs in rivers and marine sediments. Soil pH rather than the mean annual air temperature (MAAT) explains most of the observed variances of the brGDGT distribution in our soil dataset. The observed changes in the distribution of brGDGTs in the river SPM indicate that brGDGTs brought by the river to the sea are primarily derived from the lower Rhône and its tributary soils, even though in situ production in the river itself cannot be excluded. In marine surface sediments, it appears that the input of riverine brGDGTs is the primary source of brGDGTs in the Rhône prodelta, although the brGDGT composition may be further modified by the in situ production in the marine environment. More work is required to assess fully whether brGDGTs can be used to reconstruct the terrestrial paleoenvironmental changes using marine sediment cores taken in the Rhône prodelta close to the river mouth.
    Keywords: NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 3
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    (Table 1) SPM samples and sites along the Rhône Rive (2017)
    PANGAEA
    In:  Supplement to: Kim, Jung-Hyun; Buscail, Rosalyne; Fanget, Anne-Sophie; Eyrolle-Boyer, Frédérique; Bassetti, Maria Angela; Dorhout, Denise J C; Baas, Marianne; Berné, Serge; Sinninghe Damsté, Jaap S (2014): Impact of river channel shifts on tetraether lipids in the Rhône prodelta (NW Mediterranean): Implication for the BIT index as an indicator of palaeoflood events. Organic Geochemistry, 75, 99-108, https://doi.org/10.1016/j.orggeochem.2014.06.011
    Details
    Publication Date: 2023-01-13
    Description: We tested the applicability of the BIT (branched and isoprenoid tetraether) index as a proxy for palaeoflood events in the river-dominated continental margin of the Gulf of Lions (NW Mediterranean). We compared the concentrations of branched glycerol dialkyl glycerol tetraethers (br GDGTs) and crenarchaeol in suspended particulate matter (SPM) collected downstream in the Rhône River, as well as in surface sediments and a ca. 8m piston core from the Rhône prodelta. The core covered the last 400 yr, with four distinct intervals recording the river influence under natural and man-induced shifts in four main channels of the river mouth (Bras de Fer, Grand Rhône, Pégoulier and Roustan). The results indicate that there are mixed sources of br GDGTs and crenarchaeol in the prodelta, complicating application of the BIT index as an indicator of continental organic carbon input and thus as a palaeoflood proxy. However, the sedimentary BIT record for the period when ontinental material was delivered by the river more directly to the core site (Roustan phase; 1892 to the present) mimics the historical paleoflood record. This shows the potential of the BIT index as a palaeoflood proxy, provided that the delivery route of the continental material by rivers to the core sites remains constant over time. The study also highlights the idea that shifts in river channels should be taken into account for the use of the BIT index as a palaeoflood proxy.
    Keywords: Area/locality; Carbon, organic, total; Date/Time of event; DEPTH, water; Event label; Latitude of event; Longitude of event; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Rhone, France, Europe; RW1_ST1; RW2_ST2; RW3_ST4; RW4_ST3; Sample code/label; Suspended particulate matter; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 40 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 4
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    (Table 2) Concentration of CL brGDGTs and crenarchaeol for soils and marine surface sediments (2017)
    PANGAEA
    Details
    Publication Date: 2023-02-08
    Keywords: Ain, France, Europe; Branched and isoprenoid tetraether index; Branched glycerol dialkyl glycerol tetraether; Branched glycerol dialkyl glycerol tetraether, Ia; Branched glycerol dialkyl glycerol tetraether, Ib; Branched glycerol dialkyl glycerol tetraether, Ic; Branched glycerol dialkyl glycerol tetraether, IIa; Branched glycerol dialkyl glycerol tetraether, IIb; Branched glycerol dialkyl glycerol tetraether, IIc; Branched glycerol dialkyl glycerol tetraether, IIIa; Branched glycerol dialkyl glycerol tetraether, IIIb; Branched glycerol dialkyl glycerol tetraether, IIIc; Crenarchaeol; Date/Time of event; Degree of cyclisation; Delta du Rhone; DEPTH, sediment/rock; DEPTH, soil; Doubs, France, Europe; Durance, France, Europe; Elevation of event; Event label; Isere, France, Europe; Latitude of event; Location of event; Longitude of event; Lower Rhone, France, Europe; Methylation index of dominant branched tetraethers; MUC; MultiCorer; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Rhone_delta_A; Rhone_delta_AK45; Rhone_delta_B; Rhone_delta_C; Rhone_delta_D; Rhone_delta_K; Rhone_delta_L; Rhone_delta_N; RhoS-1; RhoS-10; RhoS-11; RhoS-12; RhoS-13; RhoS-14; RhoS-15-1; RhoS-15-2; RhoS-16; RhoS-17; RhoS-18; RhoS-2; RhoS-20; RhoS-21; RhoS-22-1; RhoS-22-2; RhoS-23; RhoS-24; RhoS-25; RhoS-26; RhoS-27; RhoS-28; RhoS-29-2; RhoS-3; RhoS-30; RhoS-31; RhoS-32; RhoS-33; RhoS-34; RhoS-35; RhoS-36; RhoS-37; RhoS-38; RhoS-39-1; RhoS-4; RhoS-40; RhoS-41; RhoS-42; RhoS-44; RhoS-45; RhoS-46; RhoS-47; RhoS-48; RhoS-49; RhoS-5; RhoS-50; RhoS-6; RhoS-7; RhoS-8; RhoS-9; RHS12-10; RHS12-11; RHS12-12; RHS12-13; RHS12-14; RHS12-15; RHS12-16; RHS12-17; RHS12-18; RHS12-19; RHS12-2; RHS12-20; RHS12-21; RHS12-23-b; RHS12-3; RHS12-5; RHS12-6; RHS12-7; RHS12-8; RHS12-9; Saone, France, Europe; SOIL; Soil profile; Upper Rhone, France, Europe; Upper Rhone, Switzerland, Europe
    Type: Dataset
    Format: text/tab-separated-values, 1092 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 5
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    (Table 2) Age determination of sediment core IG-KS-11 the Demerara Plateau, North Atlantic (2017)
    PANGAEA
    In:  Supplement to: Tallobre, Cédric; Loncke, Lies; Bassetti, Maria Angela; Giresse, Pierre; Bayon, Germain; Buscail, Rosalyne; de Madron, Xavier Durrieu; Bourrin, François; Vanhaesebroucke, Marc; Sotin, Christine; IGUANES Scientific Party (2016): Description of a contourite depositional system on the Demerara Plateau: Results from geophysical data and sediment cores. Marine Geology, 378, 56-73, https://doi.org/10.1016/j.margeo.2016.01.003
    Details
    Publication Date: 2023-02-08
    Description: The Demerara Plateau, belonging to the passive transform margin of French Guiana, was investigated during the IGUANES cruise in 2013. The objectives of the cruise were to explore the poorly-known surficial sedimentary column overlying thick mass transport deposits as well as to understand the factors controlling recent sedimentation. The presence of numerous bedforms at the seafloor was observed thanks to newly acquired IGUANES bathymetric, high resolution seismic and chirp data, while sediment cores allowed the characterization of the deposits covering the mass transport deposits. Modern oceanographic conditions were determined in situ, using mooring monitoring over a 10-month period. Our data indicate the presence of a Contourite Depositional System along the Demerara Plateau, most likely related to bottom current activity of the North Atlantic Deep Water (NADW). However, at the regional scale, large longitudinal waves parallel the NADW flow. Their shape and orientation seem to be inherited from interactions between bottom currents and paleomorphologies expressed at the top of mass transport deposits. Their evolution is possibly driven by the intensity of bottom current activity that might have changed over time. Overall, this work presents an integrated approach combining seismic and sedimentological evidence to study the processes at the origin of contourite formation in the Demerara Plateau. Other regional factors, such as local slope values and slope instability, also control sedimentation.
    Keywords: Age, 14C calibrated, CALIB 7.0 with MARINE13 calibration curve (Reimer et al. 2013); Age, dated; Age, dated material; Age, dated standard deviation; Atlantic Ocean; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; DEPTH, sediment/rock; IG-KSF-11; PC; Piston corer; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 39 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 6
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    (Table 3) Concentration of CL and IPL-brGDGTs and crenarchaeol for river SPM samples (2017)
    PANGAEA
    Details
    Publication Date: 2023-02-12
    Keywords: Ain_AW1; Ain, France, Europe; Branched and isoprenoid tetraether index; Branched glycerol dialkyl glycerol tetraether; Branched glycerol dialkyl glycerol tetraether, Ia; Branched glycerol dialkyl glycerol tetraether, Ib; Branched glycerol dialkyl glycerol tetraether, Ic; Branched glycerol dialkyl glycerol tetraether, IIa; Branched glycerol dialkyl glycerol tetraether, IIb; Branched glycerol dialkyl glycerol tetraether, IIc; Branched glycerol dialkyl glycerol tetraether, IIIa; Branched glycerol dialkyl glycerol tetraether, IIIb; Branched glycerol dialkyl glycerol tetraether, IIIc; Crenarchaeol; Date/Time of event; Degree of cyclisation; DEPTH, water; Doubs_DW1; Doubs, France, Europe; Durance_Du2; Durance, France, Europe; Elevation of event; Event label; Isere_IW1; Isere, France, Europe; Latitude of event; Location of event; Longitude of event; Lower Rhone, France, Europe; Methylation index of dominant branched tetraethers; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Rhone_RW1; Rhone_RW10; Rhone_RW11; Rhone_RW12; Rhone_RW13; Rhone_RW2; Rhone_RW3; Rhone_RW4; Rhone_RW5; Rhone_RW6; Rhone_RW7; Rhone_RW8; Rhone_RW9; Sample type; Saone_SW1; Saone_SW2; Saone_SW3; Saone_SW4; Saone, France, Europe; Upper Rhone, Switzerland, Europe; Water sample; WS
    Type: Dataset
    Format: text/tab-separated-values, 540 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 7
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    Benthic foraminifera in surface sediments of the Gulf of Lions
    PANGAEA
    In:  Supplement to: Schmiedl, Gerhard; de Bovée, F; Buscail, Rosalyne; Charrière, B; Hemleben, Christoph; Medernach, L; Picon, P (2000): Trophic control of benthic foraminiferal abundance and microhabitat in the bathyal Gulf of Lions, western Mediterranean Sea. Marine Micropaleontology, 40(3), 167-188, https://doi.org/10.1016/S0377-8398(00)00038-4
    Details
    Publication Date: 2023-06-27
    Description: Surface sediment was sampled at two bathyal sites in the southwestern Gulf of Lions in the western Mediterranean Sea in February and August 1997 to study the distribution and microhabitat of living (Rose Bengal stained) deep sea benthic foraminifera. Both standing stock and diversity of the faunas, and the microhabitat of distinct species mirror the trophic situation and the depth of the oxidised layer at the different sites. Our results suggest that the faunas do not comprise highly opportunistic species and are adapted to rather stable environments. In the axial channel of the Lacaze-Duthiers Canyon, organic matter fluxes are enhanced due to advective transport of organic matter resulting in elevated oxygen consumption rates in the surface sediment and a rather thin oxidised layer. The corresponding benthic foraminiferal fauna is characterised by rather high standing stock and diversity, and a well-developed deep infauna. In addition to freshly deposited phytodetritus, more degraded organic matter seems to be an important food source. In contrast, at the open slope, organic matter fluxes and oxygen consumption rates in the surface sediment are lower and the oxidised layer is much thicker than inside the canyon. The corresponding benthic foraminiferal fauna comprises mainly epifaunal and shallow-infaunal species with much lower standing stocks and clear differences between February and August. In August standing stocks are higher and the average living depths of most species shift towards the sediment surface. These differences can be attributed to patchiness or represent a seasonal trophic signal.
    Keywords: Banyuls Benthic Lander/Multicorer; BBLL; BBLL2_MC1; BBLL2_MC4; BBLL3_MC1; BBLL3_MC2; BBLM; GeoTü; Gulf of Lions; Paleoceanography at Tübingen University; SESAME; Southern European Seas: Assessing and Modelling Ecosystem Changes
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 8
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    Benthic foraminifera assemblage in sediment core BBLL2_MC1 (2000)
    PANGAEA
    Details
    Publication Date: 2023-11-09
    Keywords: Adercotryma glomeratum; Ammodiscus catinus; Ammodiscus planorbis; Ammolagena clavata; Ammoscalaria pseudospiralis; Ammoscalaria tenuimargo; Amphicoryna scalaris; Articulina tubulosa; Banyuls Benthic Lander/Multicorer; Bathysiphon sp.; BBLL; BBLL2_MC1; BBLM; Bigenerina cylindrica; Bigenerina nodosaria; Bulimina aculeata; Bulimina striata mexicana; Cassidulina laevigata; Cassidulina oblonga; Chilostomella oolina; Cibicidoides pachyderma; Counting 〉125 µm fraction; Cribrostomoides subglobosum; Crithionina spp.; Dentalina sp.; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Discammina compressa; Discorbinella bertheloti; Dry mass; Eggerelloides scaber; Foraminifera, benthic indeterminata; Gavelinopsis praegeri; GeoTü; Globobulimina affinis; Globobulimina pseudospinescens; Glomospira gordialis; Gulf of Lions; Gyroidinoides neosoldanii; Gyroidinoides orbicularis; Gyroidinoides umbonatus; Hyalinea balthica; Hyperammina laevigata; Laevidentalina flexuosa; Lagenammina tubulata; Lenticulina orbicularis; Lenticulina spp.; Lobatula lobatula; Melonis barleeanus; Nonionella opima; Paleoceanography at Tübingen University; Paracassidulina minuta; Parafissurina spp.; Planulina cf. ariminensis; Psammosphaera cf. parva; Psammosphaera fusca; Pseudotriloculina laevigata; Pyrgo murrhina; Quinqueloculina padana; Quinqueloculina venusta; Reophax spp.; Repmanina charoides; Rhabdammina; Robertinoides translucens; Saccammina sphaerica; Saccorhiza ramosa; SESAME; Sigmoilinita tenuis; Sigmoilopsis schlumbergeri; Southern European Seas: Assessing and Modelling Ecosystem Changes; Sphaeroidina bulloides; Spirillina vivipara; Spiroplectinella sagittula; Technitella legumen; Tholosina spp.; Thurammina papillata; Triloculina tricarinata; Tritaxis squamata; Trochammina cf. inflata; Uvigerina mediterranea; Uvigerina peregrina
    Type: Dataset
    Format: text/tab-separated-values, 781 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 9
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    Benthic foraminifera assemblage in sediment core BBLL3_MC2 (2000)
    PANGAEA
    Details
    Publication Date: 2023-11-09
    Keywords: Adercotryma glomeratum; Ammodiscus catinus; Ammodiscus planorbis; Ammolagena clavata; Ammoscalaria pseudospiralis; Ammoscalaria tenuimargo; Amphicoryna scalaris; Articulina tubulosa; Banyuls Benthic Lander/Multicorer; Bathysiphon sp.; BBLL; BBLL3_MC2; BBLM; Bigenerina cylindrica; Bigenerina nodosaria; Bulimina aculeata; Bulimina striata mexicana; Cassidulina laevigata; Cassidulina oblonga; Chilostomella oolina; Cibicidoides pachyderma; Counting 〉125 µm fraction; Cribrostomoides subglobosum; Crithionina spp.; Dentalina sp.; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Discammina compressa; Discorbinella bertheloti; Dry mass; Eggerelloides scaber; Foraminifera, benthic indeterminata; Gavelinopsis praegeri; GeoTü; Globobulimina affinis; Globobulimina pseudospinescens; Glomospira gordialis; Gulf of Lions; Gyroidinoides neosoldanii; Gyroidinoides orbicularis; Gyroidinoides umbonatus; Hyalinea balthica; Hyperammina laevigata; Laevidentalina flexuosa; Lagenammina tubulata; Lenticulina orbicularis; Lenticulina spp.; Lobatula lobatula; Melonis barleeanus; Nonionella opima; Paleoceanography at Tübingen University; Paracassidulina minuta; Parafissurina spp.; Planulina cf. ariminensis; Psammosphaera cf. parva; Psammosphaera fusca; Pseudotriloculina laevigata; Pyrgo murrhina; Quinqueloculina padana; Quinqueloculina venusta; Reophax spp.; Repmanina charoides; Rhabdammina; Robertinoides translucens; Saccammina sphaerica; Saccorhiza ramosa; SESAME; Sigmoilinita tenuis; Sigmoilopsis schlumbergeri; Southern European Seas: Assessing and Modelling Ecosystem Changes; Sphaeroidina bulloides; Spirillina vivipara; Spiroplectinella sagittula; Technitella legumen; Tholosina spp.; Thurammina papillata; Triloculina tricarinata; Tritaxis squamata; Trochammina cf. inflata; Uvigerina mediterranea; Uvigerina peregrina
    Type: Dataset
    Format: text/tab-separated-values, 781 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 10
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    Benthic foraminifera assemblage in sediment core BBLL2_MC4 (2000)
    PANGAEA
    Details
    Publication Date: 2023-11-09
    Keywords: Adercotryma glomeratum; Ammodiscus catinus; Ammodiscus planorbis; Ammolagena clavata; Ammoscalaria pseudospiralis; Ammoscalaria tenuimargo; Amphicoryna scalaris; Articulina tubulosa; Banyuls Benthic Lander/Multicorer; Bathysiphon sp.; BBLL; BBLL2_MC4; BBLM; Bigenerina cylindrica; Bigenerina nodosaria; Bulimina aculeata; Bulimina striata mexicana; Cassidulina laevigata; Cassidulina oblonga; Chilostomella oolina; Cibicidoides pachyderma; Counting 〉125 µm fraction; Cribrostomoides subglobosum; Crithionina spp.; Dentalina sp.; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Discammina compressa; Discorbinella bertheloti; Dry mass; Eggerelloides scaber; Foraminifera, benthic indeterminata; Gavelinopsis praegeri; GeoTü; Globobulimina affinis; Globobulimina pseudospinescens; Glomospira gordialis; Gulf of Lions; Gyroidinoides neosoldanii; Gyroidinoides orbicularis; Gyroidinoides umbonatus; Hyalinea balthica; Hyperammina laevigata; Laevidentalina flexuosa; Lagenammina tubulata; Lenticulina orbicularis; Lenticulina spp.; Lobatula lobatula; Melonis barleeanus; Nonionella opima; Paleoceanography at Tübingen University; Paracassidulina minuta; Parafissurina spp.; Planulina cf. ariminensis; Psammosphaera cf. parva; Psammosphaera fusca; Pseudotriloculina laevigata; Pyrgo murrhina; Quinqueloculina padana; Quinqueloculina venusta; Reophax spp.; Repmanina charoides; Rhabdammina; Robertinoides translucens; Saccammina sphaerica; Saccorhiza ramosa; SESAME; Sigmoilinita tenuis; Sigmoilopsis schlumbergeri; Southern European Seas: Assessing and Modelling Ecosystem Changes; Sphaeroidina bulloides; Spirillina vivipara; Spiroplectinella sagittula; Technitella legumen; Tholosina spp.; Thurammina papillata; Triloculina tricarinata; Tritaxis squamata; Trochammina cf. inflata; Uvigerina mediterranea; Uvigerina peregrina
    Type: Dataset
    Format: text/tab-separated-values, 781 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
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