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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Bahr, André; Schönfeld, Joachim; Hoffmann, Julia; Voigt, Silke; Aurahs, Ralf; Kucera, Michal; Flögel, Sascha; Jentzen, Anna; Gerdes, Axel (2013): Comparison of Ba/Ca and d18Owater as freshwater proxies: A multi-species core-top study on planktonic foraminifera from the vicinity of the Orinoco River mouth. Earth and Planetary Science Letters, 383, 45-57, https://doi.org/10.1016/j.epsl.2013.09.036
    Publication Date: 2023-07-14
    Description: Past river run-off is an important measure for the continental hydrological cycle and the as-sessment of freshwater input into the ocean. However, paleosalinity reconstructions applying different proxies in parallel often show offsets between the respective methods. Here, we compare the established foraminiferal Ba/Ca and d18OWATER salinity proxies for their capability to record the highly seasonal Orinoco freshwater plume in the eastern Caribbean. For this purpose we obtained a data set comprising Ba/Ca and d18OWATER determined on multiple spe-cies of planktonic foraminifera from core tops distributed around the Orinoco river mouth. Our findings indicate that interpretations based on either proxy could lead to different conclu-sions. In particular, Ba/Ca and d18OWATER diverge in their spatial distribution due to different governing factors. Apparently, the Orinoco freshwater plume is best tracked by Ba/Ca ratios of G. ruber (pink and sensu lato morphotypes), while d18OWATER based on the same species is more related to the local precipitation-evaporation balance overprinting the riverine freshwater contribution. Other shallow dwelling species (G. sacculifer, O. universa) show a muted response to the freshwater discharge, most likely due to their ecological and habitat prefer-ences. Extremely high Ba/Ca ratios recorded by G. ruber are attributed to Ba2+-desorption from suspended matter derived from the Orinoco. Samples taken most proximal to the freshwater source do not show pronounced Ba/Ca or d18OWATER anomalies. Here, the suspension loaded freshwater lid developing during maximum discharge suppresses foraminiferal populations. Both proxies are therefore biased towards dry season conditions at these sites, when surface salinity is only minimally reduced.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
    Publication Date: 2023-07-14
    Keywords: 222-6; 222-8_pump; 228-2_pump; 229-1_pump; 230-1_pump; 232-1_pump; 234-1_pump; 235-2_pump; 240-1_pump; 242-1_pump; 243-2_pump; 244-1_pump; 247-2; Barbados; Boca Grande Orinoco; Comment; Depth, bottom/max; Depth, top/min; DEPTH, water; Event label; Foraminifera, planktic living; Globigerinoides ruber; Globigerinoides sacculifer; Globorotalia menardii; Hand picking; Latitude of event; Longitude of event; M78/1; M78/1_222-6; M78/1_222-8-1; M78/1_228-2-1; M78/1_229-1-1; M78/1_230-1-1; M78/1_232-1-1; M78/1_234-1-1; M78/1_235-2-1; M78/1_240-1-1; M78/1_242-1-1; M78/1_243-2-1; M78/1_244-1-1; M78/1_247-2; Meteor (1986); MSN; Multiple opening/closing net; Neogloboquadrina dutertrei; Orbulina universa; Plankton pump; Plankton station 7; PP; Sample method; Volume
    Type: Dataset
    Format: text/tab-separated-values, 163 data points
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  • 3
    Publication Date: 2023-07-14
    Keywords: 219-1; 220-1; 221-1; 222-1; 236-1; 246-1; 247-1; 249-1; Barium/Calcium ratio; Boca Grande Orinoco; Bottle, Niskin; BUCKET; Bucket water sampling; Caribic; CTD/Rosette; CTD-RO; DemeraraMouth; DEPTH, water; E. Tobago, Prospector Slope; Elevation of event; EssequiboMouth; EssequiboRiver; Event label; ICP-MS, Thermo Scientific, Element 2; Identification; Latitude of event; Longitude of event; M78/1; M78/1_219-1; M78/1_220-1; M78/1_221-1; M78/1_222-1; M78/1_236-1; M78/1_246-1; M78/1_247-1; M78/1_249-1; Meteor (1986); NIS; Plankton station 3; Plankton station 4; Plankton station 6; Plankton station 7; Salinity
    Type: Dataset
    Format: text/tab-separated-values, 32 data points
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  • 4
    Publication Date: 2023-10-05
    Description: For trace element analyses, single specimens of C. wuellerstorfi have been analyzed using femtosecond laser ablation inductively coupled plasma mass spectrometry (fs-LA-ICP131 MS) at the Geochemistry Laboratory at the Max Planck Institute for Chemistry. Na, Mg, and Sr of 142 specimens of C. wuellerstorfi have been measured at high-resolution on (up to) each of the final five chambers to eliminate possible inaccuracies that are likely to be caused by varying sample size. The fs-LA-ICP-MS analyses were performed on 25-μm diameter spots on each chamber with a pulse repetition rate of 15 Hz at low fluence (0.1-0.3 J/cm2). Calibration was performed with the microanalytical synthetic reference material MACS‐3 for carbonate and NIST612 for silica. Average values of all chambers analyzed in the same specimen were used for further analyses. Since foraminifers from different regions show particular offsets in the Mg/Ca composition of their shell, depending on region specific temperature ranges of ambient seawater, region-specific formulas are used. We have applied the formula Mg/Ca=0.82e^0.19*BWT of Tisserand et al. (2013) from samples collected from similar geographic situations to avoid offsets. The formula has been applied to calculate temperature variability of each analyzed chamber. The average value obtained from chamber-to-chamber temperature variability of each specimen has been applied as average temperature data of the entire test.
    Keywords: 165-999A; Caribbean Sea; Cibicidoides wuellerstorfi, Magnesium/Calcium ratio; Cibicidoides wuellerstorfi, Sodium/Calcium ratio; Cibicidoides wuellerstorfi, Strontium/Calcium ratio; DRILL; Drilling/drill rig; Joides Resolution; LA-ICP-MS, Laser-ablation inductively coupled plasma mass spectrometer; Leg165; Sample code/label; Sample ID; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 3701 data points
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  • 5
    Publication Date: 2024-02-15
    Description: The state of a population of planktic foraminifers at a certain time reflects multiple processes in the upper ocean, including environmental conditions to which the population was exposed during its growth, the age of the cohorts, and spatiotemporal patchiness. We carried out depth-stratified (0-60, 60-100 m) replicated sampling off Puerto Rico in autumn 2012, revisiting three stations previously sampled in autumn 1994 and spring 1995, in order to analyze seasonal and interannual variability of planktic foraminifers and the stable isotopic composition of their tests. The merged dataset from all three sampling campaigns allows us to assess short- and long-term changes in foraminiferal population dynamics and the spatial assemblage coherency along the shelf edge. All three sample series cover more than 2 weeks during either spring (1995) or autumn (1994, 2012) and include the time of the full moon when reproduction of some surface-dwelling planktic foraminifers has been postulated to take place. Our analyses indicate that interannual variability affected the faunal composition, and both autumn assemblages were characterized by oligotrophic tropical species, dominated by Trilobatus sacculifer and Globigerinoides ruber (white and pink variety). However, G. ruber (white) had a higher abundance in 1994 (37 %) than in 2012 (3.5 %), which may be partially due to increasing sea surface temperatures since the 1990s. Between 60 and 100 m water depth, a different faunal composition with a specific stable oxygen isotope signature provides evidence for the presence of the Subtropical Underwater at the sampling site. Measurements on T. sacculifer sampled in autumn 2012 revealed that test size, calcification and incidence of sac-like chambers continued to increase after full moon, and thus no relation to the synodic lunar reproduction cycle was recognized. During autumn 2012, outer bands of hurricane Sandy passed the Greater Antilles and likely affected the foraminifers. Lower standing stocks of living planktic foraminifers and lower stable carbon isotope values from individuals collected in the mixed layer likely indicate the response to increased rainfall and turbidity in the wake of the hurricane.
    Keywords: 1; 2; Caribbean Sea; DATE/TIME; Depth, bottom/max; Depth, top/min; DEPTH, water; Event label; Foraminifera, planktic, shell area density; Identification; Morphotype; Planktonic foraminifera; Plankton net samples; Puerto_Rico_2012-1; Puerto_Rico_2012-2; Shell calcification intensity; Shell dimension; Shell size; Species; Station label; Trilobatus sacculifer
    Type: Dataset
    Format: text/tab-separated-values, 4241 data points
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  • 6
    Publication Date: 2024-02-02
    Keywords: 222-8; 228-2; 229-1; 230-1; 232-1; 234-1; 235-2; 240-1; 242-1; 243-2; 244-1; 246-2; 247-3; 251-1; Boca Grande Orinoco; CARIB/14; CARIB/15; CARIB/16; CARIB/17; CARIB/18; CARIB/19; CARIB/20; Caribic; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eastern Orinoco Delta; Elevation of event; Event label; GC; Giant box corer; GKG; Globigerinoides ruber pink, Barium/Calcium ratio; Globigerinoides ruber pink, Magnesium/Calcium ratio; Globigerinoides ruber pink, δ18O; Globigerinoides ruber sensu lato, Barium/Calcium ratio; Globigerinoides ruber sensu lato, Magnesium/Calcium ratio; Globigerinoides ruber sensu lato, δ18O; Globigerinoides sacculifer, Barium/Calcium ratio; Globigerinoides sacculifer, Magnesium/Calcium ratio; Globigerinoides sacculifer, δ18O; Globorotalia menardii, Barium/Calcium ratio; Globorotalia menardii, Magnesium/Calcium ratio; Gravity corer; ICP-MS, Thermo Scientific, Element 2; Latitude of event; Longitude of event; M35/1; M35/1_GKG2-1; M35/1_GKG4-1; M35/1_GKG5-3; M78/1; M78/1_222-8; M78/1_228-2; M78/1_229-1; M78/1_230-1; M78/1_232-1; M78/1_234-1; M78/1_235-2; M78/1_240-1; M78/1_242-1; M78/1_243-2; M78/1_244-1; M78/1_246-2; M78/1_247-3; M78/1_251-1; Mass spectrometer, Finnigan, MAT 253; Meteor (1986); Mg/Ca correction (Regenberg et al. 2006); MUC; MultiCorer; N. Tobago; Neogloboquadrina dutertrei, Barium/Calcium ratio; Neogloboquadrina dutertrei, Magnesium/Calcium ratio; Neogloboquadrina dutertrei, δ18O; Off Paria Peninsula; Off St. George; Off Trinidad; Orbulina universa, Barium/Calcium ratio; Orbulina universa, Magnesium/Calcium ratio; Orbulina universa, δ18O; Orinoco; Orinoco, core station 1; Orinoco, core station 3; Orinoco, core station 4; Plankton station 7; Size fraction; Temperature, calculated
    Type: Dataset
    Format: text/tab-separated-values, 1094 data points
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  • 7
    Publication Date: 2024-04-14
    Description: Here, we present a global compilation of previously reported sightings of the rare planktic foraminifer Globorotalia cavernula Bé, 1967 as well as new observations of live-collected specimens from the Southern Ocean (Subantarctic south of Africa). The goal of this synthesis is to provide the geographic and stratigraphic context needed to investigate the past and present-day distributions of this rare but possibly under-recognized species. The previous records include modern occurrences in the water column (collected by plankton net tows and a single sediment trap) and seafloor sediments ranging in age from recent to Eocene. Seafloor sediment samples were collected by dredge, sediment grabs and core-tops. Deeper sediments came from drilling cores. Existing databases provided a foundation for this compilation, particularly ForCenS for surface sediments (Siccha & Kucera, 2017) and FORCIS for water-column collections (de Garidel-Thoron et al., 2022; Chaabane et al., 2022, 2023). These records were supplemented with occurrences from the literature, PANGEA, and cruise reports of the Deep Sea Drilling Project (DSDP) / Ocean Drilling Program (ODP). Searches were conducted in October 2022 using Google Scholar, GBIF, EOL (Encyclopedia of Life, "http://eol.org", which includes records from the Smithsonian NMNH). Where available, we include information on the abundance of G. cavernula in each collection, and indicate whether photographic evidence (or drawings) could be found to support the identification. Globorotalia crozetensis Thompson, 1973 (reclassified as G. cavernula by Brummer & Kučera, 2022) and closely related Globorotalia petaliformis Boltovskoy, 1974 were also included in compilation.
    Keywords: 15-147; 154-925; 164-997A; 180-1108B; 26-253; 26-254; 26-258A; 2803; 2804; 29-284; 40-362A; 49-411A; 49-412; 54-423; 54-424; 54-425; 73-519; Abundance; abundance data; Abundance per volume; Age, comment; Antarctic Ocean/Tasman Sea/PLATEAU; ATLANTIS_II_cruise31_36; Author(s); Be67_EL_10-1-130; Be67_EL_10-1-131; Be67_EL_10-19-186; Be67_EL_10-19-187; Be67_EL_10-20-190; Be67_EL_10-2-133; Be67_EL_10-24-208; Be67_EL_10-28-219; Be67_EL_10-29-221; Be67_EL_10-31-225; Be67_EL_10-31-226; Be67_EL_10-31-227; Be67_EL_10-3-136; Be67_EL_10-32-230; Be67_EL_10-4-139; Be67_EL_10-5-141; Be67_EL_11-5-249; Be67_EL_13-1-443; Be67_EL_13-2-449; Be67_EL_13-3-456; Be67_EL_13-6-474; Be67_EL_14-4-594; Be67_EL_15-17-806; Be67_EL_15-23-843; Be67_EL_15-26-864; Be67_EL_15-5-751; Be67_EL_15-5-752; Be67_EL_17-34-1112; Be67_EL_18-1-1137; Be67_EL_18-2-1138; Be67_EL_18-3-1150; Be67_EL_19-1171; Be67_EL_19-13-1233; Be67_RC9_80; Be67_RC9_92; Be67_V16_202; BOFS31/1K; BOFS31#1; Caribbean Sea/RIDGE; CD53; Charles Darwin; Closing Discovery net, Manufacturer unknown, N70V; Comment; COMPCORE; Composite Core; Core tops; CP_trap; Cruise/expedition; Depth, description; Disc2_1951_2803; Disc2_1951_2804; DRILL; Drilling/drill rig; EL 10-1-130; EL 10-1-131; EL 10-19-186; EL 10-19-187; EL 10-20-190; EL 10-2-133; EL 10-24-208; EL 10-28-219; EL 10-29-221; EL 10-31-225; EL 10-31-226; EL 10-31-227; EL 10-3-136; EL 10-32-230; EL 10-4-139; EL 10-5-141; EL 11-5-249; EL 13-1-443; EL 13-2-449; EL 13-3-456; EL 13-6-474; EL 14-4-594; EL 15-17-806; EL 15-23-843; EL 15-26-864; EL 15-5-751; EL 15-5-752; EL 17-34-1112; EL 18-1-1137; EL 18-2-1138; EL 18-3-1150; EL 19-1171; EL 19-13-1233; ELT10; ELT11; ELT13; ELT14; ELT15; ELT17; ELT18; ELT19; Eltanin; Event label; GeoB1728-3; Giant box corer; GIK15612-2; GIK15637-1; GIK15667-1; GIK15669-2; GIK15672-2; GIK17933-2; GKG; Globorotalia cavernula; Globorotalia crozetensis; Globorotalia petaliformis; Glomar Challenger; Gravity corer (Kiel type); Hayward86_station17; Indian Ocean//PLATEAU; Indian Ocean//RIDGE; Joides Resolution; KAL; Kasten corer; Knorr73_MOC131; KOL; LATITUDE; Leg15; Leg154; Leg164; Leg180; Leg26; Leg29; Leg40; Leg49; Leg54; Leg73; LONGITUDE; M20/2; M35/1; M35027-1; M53; M53_167; M53_169; M53_172-1; M57; M6; M9; Meteor (1964); Meteor (1986); MOC; MOCNESS opening/closing plankton net; MONITOR MONSUN; Namibia Continental Margin; net tows; Nicaraguan Rise, North Atlantic Ocean; North Atlantic; North Atlantic/BASIN; North Atlantic/FRACTURE ZONE; Northeast Atlantic; North Pacific/MOUND; North Pacific/SEDIMENT POND; Number of specimens; occurrence data; Ocean and sea region; off West Africa; Optional event label; PC; Persistent Identifier; Piston corer; Piston corer (Kiel type); PLA; planktic foraminifera; Plankton net; R/V_Knorr_73_MOC131; RC08; RC08-39; RC 9-80; RC 9-92; Reference/source; Robert Conrad; S. A. Agulhas II; Sample method; Sediment cores; Sediment sample; SES; Site; SL; SO95; Solomon Sea; Sonne; South Atlantic/RIDGE; South Atlantic Ocean; South China Sea; Species; Species, unique identification; Species, unique identification (Semantic URI); Species, unique identification (URI); station 17; Trap; TRAP; Uniform resource locator/link to reference; V16; V 16-202; van Veen Grab; Vema; VGRAB; VOY016; VOY016_W2; VOY016_W3; VOY019; VOY019_M6; VOY019_M9; W2; W3
    Type: Dataset
    Format: text/tab-separated-values, 1061 data points
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