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  • Achnanthidium cf. maritimo-antarcticum; Age; AGE; Antarctica; Aulacoseira glubokoyensis; Brachysira minor; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatomella balfouriana; diatomos; Eunotia ralitsae; Fragilaria cf. capuccina; Gomphonema maritimo-antarcticum; Gomphonema sp.; Humidophila sp.; Humidophila tabellariaeformis; King George Island, Antarctica; Melosira cf. varians; Nitzschia cf. kleinteichiana; Ozon, reconstructed; ozone; Pinnularia borealis; Pinnularia cf. australomicrostauron; Pinnularia sp.; Planothidium australe; Planothidium rostrolanceolatum; Profound_Lake; proglacial lake; Psammothidium abundans; reconstructed model; SEDCO; Sediment corer; Stauroneis cf. delicata  (1)
  • Age; AGE; Arid environment; Carbon, organic, total; Carbon, organic, total, error, relative; Carbon, organic/Nitrogen, total ratio; Carbon, organic/Nitrogen, total ratio, error; Carbon and nitrogen and sulfur (CNS) isotope element analyzer, Elementar, Vario EL III; Climate change; Coastal impacts; DEPTH, sediment/rock; GC; Geochemistry; Grain size, mean; Gravity corer; Lacustrine_lagoon_THI; Lead-210 activity per mass, excess; Lead-210 activity per mass, excess, error; Morocco; Radium-226 activity per mass; Radium-226 activity per mass, error; remote sensing; Saharan wetlands; Sedimentary chlorophyll; Sedimentary chlorophyll, error; Silicon/Titanium ratio; Silicon/Titanium ratio, error; Strontium/Calcium ratio; Strontium/Calcium ratio, error  (1)
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  • 1
    Publication Date: 2023-07-18
    Description: Profound Lake (formerly known as Lago Glubokoe or Glubokoye) (62°11,066'S;058°54,413'W), is situated on Fildes Peninsula, the largest ice-free area (29 km2) of King George Island, the largest of the South Shetland Islands, located in the extreme southwestern part of the island. This lake lies 500 m from the base of the Collins glacier, close to the Uruguayan research base (Artigas) and Maxwell Bay. Morphologically it has a surface area of 90 km² and 14.7 m maximum depth. It's a holocenic, non-impacted, pro-glacial lake where diatoms are abundant and diverse. This organisms present a cell envelope, external to the plasma membrane, composed of rigid structure impregnated with silica called frustules, resistant to dissolution, that allow their preservation in sediment layers in the long term. These characteristics enable the use of diatoms in paleoenvironmental, paleoclimatic and paleoecological studies, thus we use the relative abundance of this organisms in a sediment corer in order to calibrate and evaluate the use of them as a proxy to reconstructed Ozone variability iin Antarctica.
    Keywords: Achnanthidium cf. maritimo-antarcticum; Age; AGE; Antarctica; Aulacoseira glubokoyensis; Brachysira minor; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatomella balfouriana; diatomos; Eunotia ralitsae; Fragilaria cf. capuccina; Gomphonema maritimo-antarcticum; Gomphonema sp.; Humidophila sp.; Humidophila tabellariaeformis; King George Island, Antarctica; Melosira cf. varians; Nitzschia cf. kleinteichiana; Ozon, reconstructed; ozone; Pinnularia borealis; Pinnularia cf. australomicrostauron; Pinnularia sp.; Planothidium australe; Planothidium rostrolanceolatum; Profound_Lake; proglacial lake; Psammothidium abundans; reconstructed model; SEDCO; Sediment corer; Stauroneis cf. delicata
    Type: Dataset
    Format: text/tab-separated-values, 506 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-11-02
    Description: The core was collected manually from a boat employing a gravity core sampler. The core was sliced every two centimeters in the field, packed in individual identified plastics bags, and kept refrigerated. The THI sediment core (N 27°59.139, W 12°17.109), located in the inner portion of the Lagoon, was retrieved from a secondary channel, having 52 cm of length. The salinity measured at the site on the day of the sampling was 50 PSU, thus revealing a saline gradient that increases towards the upstream, probably due to a longer residence time of the water and consequent higher evaporation rate at that site. To its right side, the secondary channel is protected by a desert plateau, while to its left lays a saltmarsh area, occupied by specimens of the genus Salicornia sp., that are periodically exposed by tidal dynamics. A low marine influence characterizes this part of the Lagoon, depths between 2.70 m and 5.20 m, during low and high tides, respectively, and surrounded by extensive heterogeneous marshes. Aiming the recognition of the environmental changes at this point of the lagoon, we have performed the following measurements in the core's sediments: dating (210Pb and 137Cs calibration), sedimentation rate, mean grainsize, Chlorophyll, Total Organic Carbon (TOC), C/N, Sr/Ca and Si/Ti elemental ratios.
    Keywords: Age; AGE; Arid environment; Carbon, organic, total; Carbon, organic, total, error, relative; Carbon, organic/Nitrogen, total ratio; Carbon, organic/Nitrogen, total ratio, error; Carbon and nitrogen and sulfur (CNS) isotope element analyzer, Elementar, Vario EL III; Climate change; Coastal impacts; DEPTH, sediment/rock; GC; Geochemistry; Grain size, mean; Gravity corer; Lacustrine_lagoon_THI; Lead-210 activity per mass, excess; Lead-210 activity per mass, excess, error; Morocco; Radium-226 activity per mass; Radium-226 activity per mass, error; remote sensing; Saharan wetlands; Sedimentary chlorophyll; Sedimentary chlorophyll, error; Silicon/Titanium ratio; Silicon/Titanium ratio, error; Strontium/Calcium ratio; Strontium/Calcium ratio, error
    Type: Dataset
    Format: text/tab-separated-values, 414 data points
    Location Call Number Limitation Availability
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