Abstract:
The dataset comprises of stratigraphic chronological and sedimentological data from Potter Peninsula, King George Island, South Shetland Islands. The data have been used to constrain deglaciation and glacier dynamics on Potter Peninsula.
Data collected in this study were funded by: Centro de Investigaciones en Ciencias de la Tierra (CICTERRA), the Direccion Nacional del Antartico/Instituto Antartico Argentino (DNA/IAA) in the framework of the Project PICTA, 2011 - 0102, IAA "Geomorfologia y Geologia Glaciar del Archipielago James Ross e Islas Shetland del Sur, Sector Norte de la Peninsula Antartica"; the Alfred Wegener Institute (AWI) research program Polar regions and Coasts in a changing Earth System (PACES II); IMCONet (FP7 IRSES, action no. 318718); the Natural Environment Research Council (NERC/BAS-CGS Grant no.81); the NERC/BAS science programmes CACHE-PEP: Natural climate variability - extending the Americas palaeoclimate transect through the Antarctic Peninsula to the pole and GRADES-QWAD: Quaternary West Antarctic Deglaciations. We thank the crews of the Argentine research station "Carlini'" and the adjoined German Dallmann-Labor (AWI) Laboratory, the Uruguayan research station "Artigas", the Russian Bellingshausen Station, the Chinese Great Wall Station, Base Presidente Eduardo Frei Montalva, the Brazilian Navy Almirante Maximiano, the UK Navy HMS Endurance and NERC/BAS James Clark Ross for logistical support during the 2006, 2011, 2014 and 2015 field seasons.
Keywords:
Deglaciation, South Shetland islands, geomorphological mapping, glacial readvance, radiocarbon dating, stratigraphy
Bentley, M., Roberts, S., Heredia Barion, P., Strelin, J., Spiegel, C., Niedermann, S., & Wacker, L. (2022). Chronological and sedimentological data from Potter Peninsula, South Shetland Islands. (Version 1.0) [Data set]. NERC EDS UK Polar Data Centre. https://doi.org/10.5285/4671a42f-7a2e-4883-948c-ef6b26dd41c9
| Access Constraints: | No restrictions apply. |
|---|---|
| Use Constraints: | Data released under Open Government Licence V3.0: http://www.nationalarchives.gov.uk/doc/open-government-licence/version/3/ |
| Creation Date: | 2022-11-27 |
|---|---|
| Dataset Progress: | Complete |
| Dataset Language: | English |
| ISO Topic Categories: |
|
| Parameters: |
|
| Personnel: | |
| Name | Michael J Bentley |
| Role(s) | Investigator |
| Organisation | Durham University |
| Name | UK Polar Data Centre |
| Role(s) | Metadata Author |
| Organisation | British Antarctic Survey |
| Name | Dr Stephen J Roberts |
| Role(s) | Investigator |
| Organisation | British Antarctic Survey |
| Name | Dr Pablo A Heredia Barion |
| Role(s) | Investigator |
| Organisation | University of Bremen |
| Name | Dr Jorge A Strelin |
| Role(s) | Investigator |
| Organisation | Centro de Investigaciones en Ciencias de la Tierra (CONICET-UNC) |
| Name | Prof Cornelia Spiegel |
| Role(s) | Investigator |
| Organisation | University of Bremen |
| Name | Dr Samuel Niedermann |
| Role(s) | Investigator |
| Organisation | Deutsches GeoForschungsZentrum GFZ |
| Name | Dr Lukas Wacker |
| Role(s) | Investigator |
| Organisation | ETH Zurich |
| Parent Dataset: | N/A |
| Reference: | Methodology: Appleby PG and Oldfield F. (1978) The calculation of lead-210 dates assuming a constant rate of supply of unsupported 210Pb to the sediment. CATENA 5: 1-8. Balco G, Stone JO, Lifton NA, Dunai TJ. (2008). A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements. Quaternary Geochronology 3: 174-195. Borchers B, Marrero S, Balco G, et al. (2016) Geological calibration of spallation production rates in the CRONUS-Earth project. Quaternary Geochronology 31: 188-198. Bronk Ramsey C. (2009) Bayesian Analysis of Radiocarbon Dates. Radiocarbon 51: 337-360. Butz C, Grosjean M, Fischer D, et al. (2015) Hyperspectral imaging spectroscopy: a promising method for the biogeochemical analysis of lake sediments. Journal of Applied Remote Sensing 9: 096031. Heaton TJ, Kohler P, Butzin M, Bard E, Reimer RW, Austin WEN, et al. (2020) Marine20-The Marine Radiocarbon Age Calibration Curve (0-55,000 cal BP). Radiocarbon 62: 779-820. Hogg AG, Heaton TJ, Hua Q, Palmer JG, Turney CSM, Southon J, et al. (2020) SHCal20 Southern Hemisphere Calibration, 0-55,000 Years cal BP. Radiocarbon 62: 759-778. Hua Q, Barbetti M, and Rakowski AZ (2013). Atmospheric radiocarbon for the period 1950-2010. Radiocarbon 55, 1-14. Lal D. (1991) Cosmic ray labelling of erosion surfaces: in situ nuclide production rates and erosion models. Earth and Planetary Science Letters 104: 424-439. Lifton N, Sato T and Dunai TJ. (2014) Scaling in situ cosmogenic nuclide production rates using analytical approximations to atmospheric cosmic-ray fluxes. Earth and Planetary Science Letters 386: 149-160. Marrero SM, Phillips FM, Borchers B, Lifton N, Aumer R and Balco G. (2016) Cosmogenic nuclide systematics and the CRONUScalc program. Quaternary Geochronology 31: 160-187. Reimer RW, and Reimer PJ. (2004). CALIBomb - calibration of post-bomb C-14 data (www.calib.org). Rein B and Sirocko F. (2002) In-situ reflectance spectroscopy - analysing techniques for high-resolution pigment logging in sediment cores. International Journal of Earth Sciences 91: 950-954. Stone JO. (2000) Air pressure and cosmogenic isotope production. Journal of Geophysical Research: Solid Earth 105: 23753-23759. Sugden DE and John BS. (1973) The ages of glacier fluctuations in the South Shetland Islands, Antarctica. In: van Zinderen; Bakker EM (ed) Palaeoecology of Africa, the Surrounding Islands and Antarctica. Balkema, Cape Town, 141-159. Associated paper: Heredia Barion, P.A., Strelin, J.A., Roberts, S.J., et al. (2022). The impact of Holocene deglaciation and glacial dynamics on the landscapes and geomorphology of Potter Peninsula, King George Island (Isla 25 Mayo), NW Antarctic Peninsula. Frontiers in Earth Science https://doi.org/10.3389/feart.2022.1073075 |
|
|---|---|---|
| Quality: | Pre-bomb calibrated ages have been rounded to the nearest 10 years, and to the nearest hundred years in the manuscript text to reflect realistic total (internal and external) uncertainties. Post-bomb ages have been rounded to the nearest year. | |
| Lineage: | Mapping and Stratigraphic section sample collection Mapping was undertaken in ARC-GIS, with final layouts achieved in Adobe Illustrator v. 26.2.1 or CorelDRAW v. 2020. Lithostratigraphic descriptions and radiocarbon sampling were undertaken at an outer peninsula stratigraphic profile referred to as "new Pingfo II" and a new river section adjacent to the 'Potter Cove section' sampled by Sugden and John (1973). We also sampled terrestrial moss samples for radiocarbon dating from a recently exposed 'Inland outcrop' which is located inside the 1956 CE limit, around 700 m from the active glacier front. The stratigraphic sections were characterised using textural criteria, fabric, composition, sedimentary structures, and grain size analysis to determine the relationships between different depositional units. Radiocarbon (C-14) dating Twenty-one Accelerator Mass Spectrometry (AMS) radiocarbon (C-14) ages were obtained from seaweed, marine mollusc shells, penguin and undetermined bones, remnants of terrestrial mosses embedded in stratigraphic profiles and moraine sediments. Calibration of marine sample radiocarbon ages (marine shells and seaweed) was undertaken in Oxcal v. 4.4 using the Marine20 calibration curve (Bronk Ramsey, 2009; Heaton et al., 2020), and a newly recalculated local marine reservoir age offset (delta R) of 666 plus-minus 76 C-14 years (Heaton et al., 2020), which represents the weighted mean delta R of four radiocarbon-dated marine samples collected prior to 1950 CE from the northern Antarctic Peninsula and Signy Island in the online Marine20 database (http://calib.org/marine/). Terrestrial and aquatic moss samples were calibrated using the Southern Hemisphere SHCal20 calibration curve in Oxcal v. 4.4 (Hogg et al., 2020). Post-bomb (more than 1950 CE) ages were corrected according to 13C/12C isotopic ratios from measured pMC with the 'present day' pMC value defined as 107.5 percent (2010 CE) and calibrated using the SHCal13 SH Zone 1-2 Bomb curve in CALIBomb (Reimer and Reimer, 2004; Hua et al., 2013). Cosmogenic Helium-3 (He-3) nuclide surface exposure dating (CSED). Five samples were collected for He-3 CSED using a hammer and chisel to remove the upper few centimetres of exposed surfaces. Differential GPS (dGPS) measurements were undertaken using a Trimble Pathfinder ProXH to determine the precise location and altitude of boulders in relation to the landmark DALL 66019M002 (62.23787 degrees S, 58.66455 degrees W, ellipsoidal height 39.376 m) triangulation station located on the Argentine Carlini base, a few hundred metres away from the sampled erratics. dGPS precision is better than 10 cm in all axes, but ellipsoid correction errors are larger. Exposure ages were calculated using the CRONUScalc calculator (Version 2.0; Marrero et al., 2016) with the time-dependent Lal (1991)/Stone (2000) scaling model (Lm) for altitude at Antarctic pressure conditions and the primary calibration data set for He-3 in pyroxene, which yields a long term sea-level high latitude (SLHL) scaled production rate of 122 plus-minus 13 at g-1 a-1 (Borchers et al., 2016). External age uncertainties include production rate uncertainties. Exposure ages determined with other scaling models (e.g., Lifton et al., 2014) vary by up to around 6 percent. We report internal and external uncertainties. Following Balco et al. (2008), external uncertainties are used for comparison with calibrated AMS radiocarbon ages and error ranges. Grain size analysis Thirteen samples were dry sieved to separate the fraction larger than 2 mm, placed in an ultrasonic bath for 10 seconds, then placed in a reciprocating shaker and left overnight. Samples were wet sieved to separate the fraction less than 0.063 mm (silt and clay size), and the coarser fraction was dried in an oven at 50 degrees Celsius and dry sieved into sand fractions (more than 1mm, more than 0.5 mm, more than 0.25 mm, more than 0.125 mm and more than 0.063 mm). The silt and clay fractions were transferred to a sedimentation cylinder and fine and coarse silt separated from clays after settling using the pipette method. The clay fraction was then concentrated using a centrifuge, and all fractions were dried in an oven at 40 degrees Celsius. Additional statistical analysis was undertaken, and figures constructed, using R v. 4.1.0/RStudio v. 1.4.1717 (primarily packages Tidyverse, ggplot2, Vegan, Rioja, Ggally v. 2.1.2, RBacon, Rcarbon, Bchron), Sigmaplot v. 14.0, C2 (Juggins, 2007), MATLAB v. R2021a, with final layouts achieved in Adobe Illustrator v. 26.2.1 or CorelDRAW v. 2020. Code, data, all packages used and package references can be found at: https://github.com/stever60/Potter Peninsula |
|
| Temporal Coverage: | |
|---|---|
| Start Date | 2011-11-01 |
| End Date | 2011-11-30 |
| Spatial Coverage: | |
| Latitude | |
| Southernmost | -62.2473 |
| Northernmost | -62.2389 |
| Longitude | |
| Westernmost | -58.6729 |
| Easternmost | -58.6466 |
| Altitude | |
| Min Altitude | N/A |
| Max Altitude | N/A |
| Depth | |
| Min Depth | N/A |
| Max Depth | N/A |
| Location: | |
| Location | Antarctica |
| Detailed Location | Potter Peninsula, South Shetland Islands |
| Data Collection: | Radiocarbon samples were prepared at the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research and British Antarctic Survey. AMS measurements were undertaken at ETH Zurich and Beta Analytical, Miami, and 13C/12C isotope ratios were used to calculate Conventional Radiocarbon Ages. |
|---|
| Data Storage: | This entry contains the following data files (in alphabetical order): Potter C14 data.csv - radiocarbon ages from stratigraphic sections on Potter Cove Potter Cove fly around.mov - 3D fly-past video showing the location of key sites Potter GrainSize.csv - grain size data for the new Pingfo-II section Potter He3 cosmogenic data.csv - data for cosmogenic exposure dating analysis |
|---|