Palaeoclimatic implications of the occurrence of the arcoid bivalve Anadara trapezia (Deshayes) in the Quaternary of Australasia

Murray-Wallace, Colin V.; Beu, A. G.; Kendrick, George W.; Brown, L. J.; Belperio, A.P.; Sherwood, John E.

doi:10.1016/s0277-3791(99)00015-3

Cited by 71 publications

(41 citation statements)

References 86 publications

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“…125 Ma (MIS 5e). This evidence is consistent with the presence of Anadara trapezia and a significant number of other warm water molluscan immigrants to New Zealand waters at these times (Murray-Wallace et al 2000;Beu 2004). …”

Section: Implications For Faunal Historysupporting

confidence: 83%

A New Zealand climatic template back to c. 3.9 Ma: ODP Site 1119, Canterbury Bight, south‐west Pacific Ocean, and its relationship to onland successions

Carter

2005

Journal of the Royal Society of New Zealand

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Ocean Drilling Program Site 1119 is located east of South Island, New Zealand, in 394 m water depth on the upper continental slope. Though 93 km offshore today, during recent glaciations the site lay near the lowstand shoreline, directly beneath the path of seasonal riverine meltwater plumes. The core comprises an upper portion (0-86.19 metres composite depth (mcd)) deposited as upper slope clinoforms and a lower portion (to 513.5 mcd) deposited as mid-slope, intermediate water depth sediment drifts, the two intervals being separated across a short c. 25 k.y. long unconformity within Marine Isotope Stage (MIS) 8. Almost throughout, the core comprises alternating micaceous muds and silts (glacials) and muddy, sometimes calcareous, sands (interglacials). Because of the enhanced potassium content of the terrigenous muds, the lithologies that characterise the two different climatic states possess markedly different natural gamma radiation signals, high and low, respectively. The natural gamma profile of Site 1119 therefore provides a high quality climatic time series with a 1-2 k.y. resolution (as sampled) back to the mid-Pliocene. The cyclic gamma ray pattern provides a proxy measure of ice volume in the Southern Alps, and is therefore an atmospheric record. This record matches closely that of oceanic oxygen isotope curves back to MIS 100 (2.4 Ma) and less closely beyond to MIS Gi-11 (3.91 Ma) at the base of the core. Marked, high gamma ray intervals at 3.68-3.63, 3.38, 3.12, and 2.80-2.67 Ma may reflect sharp mid-latitude atmospheric coolings at these times, as supported by marine faunal and isotopic evidence elsewhere in the New Zealand region. Alternatively, they may in part reflect changes in clay provenance consequent upon tectonic uplift in the hinterland. The natural gamma measurements are consistent with an overall decline of 6°C in average atmospheric temperature over South Island, New Zealand, since 2.45 Ma. Milankovitch 41 k.y. cyclicity is also prominent in the natural gamma record over this period, and its 60 API unit magnitude implies temperature swings up to 12°C between glacials and interglacials (G/I). Similarly large G/I temperature changes occur also in nearby sea surface temperatures east of South Island and in atmospheric temperatures in Antarctica (Vostok), suggesting that Pleistocene climate signals were closely synchronised across wide areas of Southern Hemisphere middle and high latitudes. Together with changing tectonic and related palaeogeographic patterns, these temperature changes must have played a significant role in influencing the local time ranges of taxa used in biostratigraphy. Very few, if any, traditional New Zealand Pliocene-Pleistocene index fossils have synchronous ranges across the region, and other methods of correlation (magnetostratigraphy, cyclostratigraphy, tephrochronology, isotope stratigraphy, and numeric dating) Zealand, Volume 35, 2005 have therefore come to be of particular importance. The Site 1119 natural gamma record provides a unique reference te...

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Section: Implications For Faunal Historysupporting

confidence: 83%

A New Zealand climatic template back to c. 3.9 Ma: ODP Site 1119, Canterbury Bight, south‐west Pacific Ocean, and its relationship to onland successions

Carter

2005

Journal of the Royal Society of New Zealand

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“…For the purposes of this study, I therefore assume that the A. trapezia specimens were live-collected in October-November 1904. A. trapezia is common on intertidal mudflats in southeast Australia and is strongly associated with the presence of seagrasses (Inglis 1992;Murray-Wallace et al 2000;Sullivan 1961). The small size of the four individual specimens (11.5g, 4.3g, 4.6g, 4.5g) led to the adoption of the same dating strategy as that for V. singaporina (see above).…”

Section: Live-collected Known-age Samplesmentioning

confidence: 99%

Coastal Themes: An Archaeology of the Southern Curtis Coast, Queensland : An Archaeology of the Southern Curtis Coast, Queensland

Ulm¹

2006

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terra australis 24Terra Australis reports the results of archaeological and related research within the south and east of Asia, though mainly Australia, New Guinea and island Melanesia -lands that remained terra australis incognita to generations of prehistorians. Its subject is the settlement of the diverse environments in this isolated quarter of the globe by peoples who have maintained their discrete and traditional ways of life into the recent recorded or remembered past and at times into the observable present.Since the beginning of the series, the basic colour on the spine and cover has distinguished the regional distribution of topics as follows: ochre for Australia, green for New Guinea, red for South-East Asia and blue for the Pacific Islands. From 2001, issues with a gold spine will include conference proceedings, edited papers and monographs which in topic or desired format do not fit easily within the original arrangements. All volumes are numbered within the same series. List of volumes in Terra AustralisVolume 1: Burrill Lake and Currarong: Coastal Sites in Southern New South Wales. R.J. Lampert (1971) Volume 2: Ol Tumbuna: Archaeological Excavations in the Eastern Central Highlands, Papua New Guinea. J.P. White (1972) Volume 3 994.01Copyright of the text remains with the contributors/authors, 2006. This book is copyright in all countries subscribing to the Berne convention. Apart from any fair dealing for the purpose of private study, research, criticism or review, as permitted under the Copyright Act, no part may be reproduced by any process without written permission. Inquiries should be made to the publisher. THE RESEARCH DOCUMENTED here represents the first systematic archaeological work in this area of the southeast Queensland coast and was undertaken as a major part of a larger, multicomponent project concerning archaeology and cultural heritage in the traditional country of Gooreng Gooreng speaking people. Sean's task was to build upon the results of exploratory site survey and excavation to address two key concerns. The first was the relationship of patterns of cultural change in his study area to those described elsewhere in southeast Queensland. The second was to ensure that any such comparisons were taphonomically well-founded, particularly with regard to the analytical integrity of the shell middens upon which he and other coastal researchers in Australia rely so heavily. Sean took to this task with a vengeance, closely surveying a large area of landscape and excavating an array of site types to provide himself with a solid sample of the archaeological variation thus revealed. Though most were not archaeologically rich, these sites provided substantial grist for Sean's taphonomic mill, prompting him to adapt conjoining techniques to work on bivalve shellfish -a simple but clever innovation -as well as to undertake much more sophisticated work on local variation in correction factors for the radiocarbon dating of marine shell. In the end, he was able to distil the three-phase cul...

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“…The coastal successions contain similar faunal assemblages to the subsequent interglacial (Last Interglacial Maximum; OISs 5e: 125 ka). In particular, elements of a warmer water fauna appear in the estuarine and peritidal facies of southern Australia and include Anadara trapezia and the megascopic foraminifer Marginopora vertebralis (Cann and Clarke, 1993;Murray-Wallace et al, 2000). The absence of these species in much of southern and Western Australia in the present, Holocene interglacial has been attributed to a significant reduction in estuarine environments resulting from reduced freshwater input to estuaries.…”

Section: Middle Pleistocene Coastal Successions and Sea-levelsmentioning

confidence: 99%

Pleistocene coastal stratigraphy, sea‐level highstands and neotectonism of the southern Australian passive continental margin—a review

Murray-Wallace

2002

J Quaternary Science

162

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Murray-Wallace, C. V. 2002. Pleistocene coastal stratigraphy, sea-level highstands and neotectonism of the southern Australian passive continental margin-a review.ABSTRACT: Located in a tectonically stable, intraplate setting and in the far field of former ice sheets, the southern Australian passive continental margin represents a globally important region for quantifying sea level during Pleistocene highstands. The stratigraphical record of the southern Australian margin is dominated by geographically extensive coastal barrier, estuarine and peritidal landforms of bioclastic, temperate carbonate affinity, a function of regional aridity. Siliciclastic successions dominate the eastern Australian coastline. Despite the generally high level of tectonic stability, regional contrasts are evident in the elevation of Pleistocene shoreline deposits that largely relate to pre-Quaternary geotectonic setting. The most complete record of Pleistocene highstand deposits occurs in the Murray Basin-Coorong Coastal Plain region, and indicates that interglacial sea-level highstands, for at least the past 11 interglacials, did not deviate by more than 6 m from present sea-level. The Pleistocene marginal marine record of southern Australia is dominantly represented by coastal successions deposited during marine oxygen isotope stages 5e and 7, equating with relative sea-level maxima of 2-6 m and greater than 1 m above present sea-level (APSL) respectively. Intertidal facies of Late Pleistocene interstadial successions rarely occur above present sea level. The most reliable record of glacio-eustatic (ice equivalent) sea level is registered on coastlines developed on stable Precambrian cratons such as the Gawler Craton (Eyre Peninsula), where a consistent elevation of 2 m APSL is registered for over 500 km for the last interglacial shoreline (125 ka).

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Palaeoclimatic implications of the occurrence of the arcoid bivalve Anadara trapezia (Deshayes) in the Quaternary of Australasia

Cited by 71 publications

References 86 publications

A New Zealand climatic template back to c. 3.9 Ma: ODP Site 1119, Canterbury Bight, south‐west Pacific Ocean, and its relationship to onland successions

A New Zealand climatic template back to c. 3.9 Ma: ODP Site 1119, Canterbury Bight, south‐west Pacific Ocean, and its relationship to onland successions

Coastal Themes: An Archaeology of the Southern Curtis Coast, Queensland : An Archaeology of the Southern Curtis Coast, Queensland

Pleistocene coastal stratigraphy, sea‐level highstands and neotectonism of the southern Australian passive continental margin—a review

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