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  • 1
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract The north-east Australian margin is the largest modern example of a tropical mixed siliciclastic/carbonate depositional system, with an outer shelf hosting the Great Barrier Reef (GBR) and an inner shelf dominated by fluvially sourced siliciclastic sediment wedges. The long-term interplay between these sediment components and sea level is recorded in the Queensland Trough, a 1–2 km deep N–S elongate basin situated between the GBR platform and the Queensland Plateau. In this paper, 154 samples from 45 surface grabs and six well-dated piston cores were analysed for total carbonate content, carbonate mineralogy and Sr concentration to establish spatial and temporal patterns of carbonate accumulation in the Queensland Trough over the last 300 kyr. Surface carbonate contents are lowest on the inner-shelf (〈5%) and in the trough axis (〈60%) because of siliciclastic dilution. Carbonate on the shelf is mostly Sr-rich aragonite and high-Mg calcite (HMC), whereas that in the basin is mostly low-Mg calcite. Once normalized to remove the effects of siliciclastic dilution, surface Sr-rich aragonite and HMC abundances decrease linearly to background levels ≈ 100 km seaward of the shelf edge. Core samples show that, over time, normalized aragonite and Sr abundances are greatest during periods of shelf flooding and lowest when sea level drops below the shelf edge. This is consistent with changes in the production of coral and calcareous algae, and the shedding of their debris from the shelf. Interestingly, normalized HMC concentrations on the slope peak during periods of major transgression, perhaps because of maximum off-shelf transport from inter-reef areas or intermediate water dissolution. After accounting for siliciclastic dilution, there are strong similarities in both spatial and temporal patterns of carbonate minerals between slopes and basins of the north-east Australian margin and those of pure carbonate margins such as the Bahamas. A limited set of basic processes, including the formation and breakdown of carbonate on the shelf, the transport of carbonate off the shelf and eustatic sea level, probably controls carbonate accumulation in slope and basin settings of tropical environments, irrespective of proximal siliciclastic sediment sources.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Between 34 and 15 million years (Myr) ago, when planetary temperatures were 3–4 °C warmer than at present and atmospheric CO2 concentrations were twice as high as today, the Antarctic ice sheets may have been unstable. Oxygen isotope records from deep-sea ...
    Type of Medium: Electronic Resource
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  • 3
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    PANGAEA
    In:  Supplement to: Gagan, Michael K; Dunbar, Gavin B; Suzuki, Atsushi (2012): The effect of skeletal mass accumulation in Porites on coral Sr/Ca and d18O paleothermometry. Paleoceanography, 27(1), PA1203, https://doi.org/10.1029/2011PA002215
    Publication Date: 2023-05-12
    Description: Paleotemperature estimates based on coral Sr/Ca have not been widely accepted because the reconstructed glacial-Holocene shift in tropical sea-surface temperature (~4-6°C) is larger than that indicated by foraminiferal Mg/Ca (~2-4°C). We show that corals over-estimate changes in sea-surface temperature (SST) because their records are attenuated during skeletogenesis within the living tissue layer. To quantify this process, we microprofiled skeletal mass accumulation within the tissue layer of Porites from Australasian coral reefs and laboratory culturing experiments. The results show that the sensitivity of the Sr/Ca and d18O thermometers in Porites will be suppressed, variable, and dependent on the relationship between skeletal growth rate and mass accumulation within the tissue layer. Our findings help explain why d18O-SST sensitivities for Porites range from -0.08 per mil/°C to -0.22 per mil/°C and are always less than the value of -0.23 per mil/°C established for biogenic aragonite. Based on this observation, we recalibrated the coral Sr/Ca thermometer to determine a revised sensitivity of -0.084 mmol/mol/°C. After rescaling, most of the published Sr/Ca-SST estimates for the Indo-Pacific region for the last ~14,000 years (-7°C to +2°C relative to modern) fall within the 95% confidence envelope of the foraminiferal Mg/Ca-SST records. We conclude that two types of calibration scales are required for coral paleothermometry; an attenuated Porites-specific thermometer sensitivity for studies of seasonal to interannual change in SST and, importantly, the rescaled -0.084 mmol/mol/°C Sr/Ca sensitivity for studies of 20th-century trends and millennial-scale changes in mean SST. The calibration-scaling concept will apply to the development of transfer functions for all geochemical tracers in corals.
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 4
    Publication Date: 2023-01-30
    Description: Quantification of ice-rafted debris (IRD) abundances in deep-sea records using three independent methodologies of obtaining IRD abundances and how different approaches will affect determinations of mass accumulation rates (MARs). The three methodologies for this cross comparison of methods include: counting clasts 〉2 mm in x-radiograph images; the sieved weight percentage of the medium-to-coarse sand fraction (250 μm-2 mm); and volumetric estimates of the 〉125 μm sand fraction using Laser diffraction Particle Size Analysis (LPSA) methods to determine particle size. The data are collected from the Wilkes Land and Ross Sea region of Antarctica, using cores RS15-LC42,RS15-LC48, IODP sites 1361 and ODP site 1165.
    Keywords: Antarctica; Grain Size; Ice Rafted Debris; method
    Type: Dataset
    Format: application/zip, 15 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Grant, Georgia Rose; Naish, Timothy R; Dunbar, Gavin B; Stocchi, Paolo; Kominz, Michelle A; Kamp, Peter J; Tapia, C A; McKay, Robert M; Levy, Richard H; Patterson, Molly O (2019): The amplitude and origin of sea-level variability during the Pliocene epoch. Nature, https://doi.org/10.1038/s41586-019-1619-z
    Publication Date: 2023-01-30
    Description: Earth is heading towards a climate that was last experienced more than 3 Myr during the “mid-Pliocene warm period”1. Atmospheric carbon dioxide (pCO2) concentrations were ~400 ppm, global sea level oscillated in response to orbital forcing2,3 and peak global mean sea level (GMSL) may have reached ~20 m above present4,5. For sea-level rise of this magnitude extensive retreat or collapse of the Greenland, West Antarctic and marine based sectors of the East Antarctic ice sheets are required. Yet the relative amplitude of sea-level variations within glacial-interglacial cycles remains poorly-constrained. Here, we show sea-level varied on average by 13 ± 5 m over glacial-interglacial cycles during the mid- to late Pliocene, ~3.3 - 2.5 Myrs. We calibrated a theoretical relationship between modern sediment transport by waves and water depth and then applied the technique to Pliocene grain size in shallow-marine sediments from Whanganui Basin, New Zealand, thereby estimating past sea level variation. The resulting PlioSeaNZ record is independent of the deep ocean oxygen isotope (δ18O) record for global ice volume3, and in phase with ~20 kyr duration cycles of insolation over Antarctica, paced by eccentricity-modulated orbital precession between 3.3 and 2.7 Ma6. Thereafter, sea-level fluctuations are paced by ~41 kyr cycles in Earth's axial tilt as ice sheets stabilise on Antarctica and intensify in the northern hemisphere3,6. Sensu stricto, we provide the amplitude of relative sea-level (RSL) change, rather than absolute GMSL change. However, glacio-isostatic adjustment (GIA) simulations of RSL change, show that the PlioSeaNZ record approximates eustatic sea level (ESL), defined here as GMSL unregistered to the centre of the Earth. Nonetheless, under conservative assumptions, our estimates limit maximum Pliocene sea level to less than +25 m and provide new constraints on polar ice-volume variability under climate conditions Earth is on track to experience this century.
    Keywords: File format; File name; File size; mid-Pliocene warm period; Paleoclimate; Paleo-Sea Level; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 6
    Publication Date: 2023-05-12
    Keywords: Date; DIVER; Environment; Event label; Extension rate; Java; Latitude of event; Longitude of event; Ningaloo_Reef; Ningaloo Reef, lagoon; Nusa_Barung; Orpheus_1995; Orpheus Island, Australia; Philippines; Samar; Sample code/label; Sampling by diver; Species; Temperature, water; Thickness
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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  • 7
    Publication Date: 2023-06-27
    Keywords: 14.2 km at 096° true from Cape Roberts; Cape Roberts Project; Core wireline system; CRP; CRP-2; CWS; DEPTH, sediment/rock; Mode, grain size; off Cape Roberts, Ross Sea, Antarctica; Particle size analyser; Sampling/drilling from ice; Sand; Sand, mean; Standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 672 data points
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  • 8
    Publication Date: 2023-06-27
    Keywords: Cape Roberts Project; Core wireline system; CRP; CRP-3; CWS; DEPTH, sediment/rock; Mode, grain size; Particle size analyser; Ross Sea; Sampling/drilling from ice; Sand; Sand, mean; Standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 1608 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Naish, Tim R; Barrett, Peter J; Dunbar, Gavin B; Woolfe, Ken; Dunn, A G; Henrys, Stuart A; Claps, Michele; Powell, Ross; Fielding, Christopher R (2001): Sedimentary cyclicity in CRP drillcore, Victoria Land Basin, Antarctica. Terra Antartica, 8(3), 225-244, hdl:10013/epic.28205.d001
    Publication Date: 2023-06-27
    Description: The upper 1200 m of pre-Pliocene sediment recovered by Cape Roberts Project (CRP) drilling off the Victoria Land coast of Antarctica between 1997-1999 has been subdivided into 54 unconformity-bound stratigraphic sequences, spanning the period c. 32 to 17 Ma. The sequences are recognised on the basis of the cyclical vertical stacking of their constituent lithofacies, which are enclosed by erosion surfaces produced during the grounding of the advancing ice margin onto the sea floor. Each sequence represents deposition in a range of offshore shelf to coastal glacimarine sedimentary environments during oscillations in the ice margin across the Western Ross Sea shelf, and coeval fluctuations in water depth. This paper applies spectral analysis techniques to depth- and time-series of sediment grain size (500 samples) for intervals of the core with adequate chronological data. Time series analysis of 0.5-l.0m-spaced grainsize data spanning sequences 9-11 (CRP-2/2A) and sequences 1-7 (CRP-3) suggests that the length of individual sequences correspond to Milankovitch frequencies, probably 41 k.y., but possibly as low as 100 k.y. Higher frequency periodic components at 23 k.y. (orbital precession) and 15-10 k.y. (sub-orbital) are recognised at the intrasequence-scale, and may represent climatic cycles akin to the ice rafting episodes described in the North Atlantic Ocean during the Quaternary. The cyclicity recorded by glacimarine sequences in CRP core provides direct evidence from the periphery of Antarctica for orbital oscillations in the size of the Oligocene-Early Miocene East Antarctic Ice Sheet.
    Keywords: 14.2 km at 096° true from Cape Roberts; Cape Roberts Project; Core wireline system; CRP; CRP-2; CRP-3; CWS; off Cape Roberts, Ross Sea, Antarctica; Ross Sea; Sampling/drilling from ice
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Marr, Julene P; Baker, Joel A; Carter, Lionel; Allan, Adrian S R; Dunbar, Gavin B; Bostock, Helen C (2011): Ecological and temperature controls on Mg/Ca ratios of Globigerina bulloides from the southwest Pacific Ocean|. Paleoceanography, 26(2), PA2209, https://doi.org/10.1029/2010PA002059
    Publication Date: 2023-05-12
    Description: We present Mg/Ca data for Globigerina bulloides from 10 core top sites in the southwest Pacific Ocean analyzed by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS). Mg/Ca values in G. bulloides correlate with observed ocean temperatures (7°C-19°C), and when combined with previously published data, an integrated Mg/Ca-temperature calibration for 7°C-31°C is derived where Mg/Ca (mmol/mol) = 0.955 * e**(0.068 * T) (r**2 = 0.95). Significant variability of Mg/Ca values (20%-30%) was found for the four visible chambers of G. bulloides, with the final chamber consistently recording the lowest Mg/Ca and is interpreted, in part, to reflect changes in the depth habitat with ontogeny. Incipient and variable dissolution of the thin and fragile final chamber, and outermost layer concomitantly added to all chambers, caused by different cleaning techniques prior to solution-based ICPMS analyses, may explain the minor differences in previously published Mg/Ca-temperature calibrations for this species. If the lower Mg/Ca of the final chamber reflects changes in depth habitat, then LA-ICPMS of the penultimate (or older) chambers will most sensitively record past changes in near-surface ocean temperatures. Mean size-normalized G. bulloides test weights correlate negatively with ocean temperature (T = 31.8 * e**(-30.5*wtN); r**2 = 0.90), suggesting that in the southwest Pacific Ocean, temperature is a prominent control on shell weight in addition to carbonate ion levels.
    Type: Dataset
    Format: application/zip, 2 datasets
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