James Shulmeister

University of Canterbury

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Jie Chang

Chinese Academy of Sciences

David Fink

Australian Nuclear Science and Technology Organisation

Tammy M. Rittenour

Utah State University

Glenn D. Thackray

Idaho State University

Allen Gontz

Clarkson University

Enlou Zhang

Chinese Academy of Sciences

Nicholas R. Patton

Idaho State University

Daniel Ellerton

University of Queensland

Olivia M. Hyatt

University of Canterbury

Weiwei Sun

Nanjing Institute of Geography and Limnology

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Faculty of 1000 (United States)

106

National University of Tierra del Fuego

101

University of Queensland

Chinese Academy of Sciences

University of Canterbury

Australian National University

Environmental Earth Sciences

Centre National de la Recherche Scientifique

University of Wollongong

Victoria University of Wellington

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QUA volume 87 issue 3 Cover and Front matter

Quaternary Research (2017)

Derek B. Booth Nicholas Lancaster Lewis A. Owen Patrick J. Bartlein Robert K. Booth

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Front cover

Content (measure theory)

10.1017/qua.2017.44

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Variations in wave climate as a driver of shoreline change in southeast Queensland, Australia

AGU Fall Meeting Abstracts (2018)

Sarah McSweeney James Shulmeister

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Beach cusp morphology on sand and mixed sand and gravel beaches, South Island, New Zealand

Marine Geology (1999)

Thomas J. Nolan R. M. Kirk James Shulmeister

Elevation (ballistics)

Plage

10.1016/s0025-3227(98)00150-9

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Citations (50)

Corrigendum to “Formation and evolution of the Holocene massive landslide-dammed lakes in the Jishixia Gorges along the upper Yellow River: No relation to China’s Great Flood and the Xia Dynasty” [Quat. Sci. Rev. 218 (2019) 267–280]

Quaternary Science Reviews (2020)

Yuzhu Zhang Chun Chang Huang James Shulmeister Yongqiang Guo Tao Liu

Three gorges

Legend

10.1016/j.quascirev.2020.106405

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The Holocene evolution of a well nourished gravelly barrier and lagoon complex, Kaitorete “Spit”, Canterbury, New Zealand

Marine Geology (1997)

Jane M. Soons James Shulmeister SARAH B. HOLT

Peninsula

10.1016/s0025-3227(97)00003-0

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Citations (42)

Geomorphology of the Inskip Peninsula, Queensland, Australia

Journal of Maps (2019)

Martin Köhler James Shulmeister

The Inskip Peninsula is the link between two major coastal dune fields; Fraser Island (the world’s largest sand island) and the adjacent Cooloola Sand Mass. There has been a notable lack of research into the geomorphology of the sand masses and the relationship between the two dunefields. This paper presents a detailed geomorphological map of the Inskip Peninsula at a scale of 1:10,000. The Peninsula can be divided into three parts; an eastern section dominated by late Holocene strandlines and foredunes with an active spit at the northern limit of the peninsula; a central zone composed of broader foredune ridges and swales and an eastern zone comprised of remnants of older parabolic sand dunes and foredune remnants. The map provides a framework for ongoing work on landscape reconstruction.

Foredune

Peninsula

Sand dune stabilization

10.1080/17445647.2019.1568314

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Citations (1)

Issue Information

Geoarchaeology (2016)

Jaafar Jotheri M. Allen T. J. Wilkinson Benjamin T. Pennington Judith Bunbury

3,261 (US), US$3,408 (Canada and Mexico), £1,779 (UK), €2,244 (Europe), US$3,480 (Rest of World).Prices are exclusive of tax.Asia-Pacific GST, Canadian GST/HST, and European VAT will be applied at the appropriate rates.For more information on

10.1002/gea.21577

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A Holocene Record of Human Induced and Natural Environmental Change from Lake Forsyth (Te Wairewa), New Zealand

Journal of Paleolimnology (2005)

Craig Woodward James Shulmeister

Deforestation

Limnology

10.1007/s10933-005-5708-7

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Enhanced solar activity influence on the summer temperature variability of the southeast margin of the Qinghai-Tibetan Plateau in the late Holocene

EGU General Assembly Conference Abstracts (2017)

Jie Chang Enlou Zhang Enfeng Liu James Shulmeister

Solar variation

Margin (machine learning)

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A Holocene record of climate and hydrological changes from Little Llangothlin Lagoon, south eastern Australia

The Holocene (2014)

Craig Woodward James Shulmeister Dorothy Bell Robert Haworth Geraldine Jacobsen

We present a new well dated Holocene record of environmental change from Little Llangothlin Lagoon in eastern Australia derived from aquatic plant macrofossils, macroscopic charcoal flux, and sediment stratigraphy from multiple cores. Little Llangothlin was an ephemeral freshwater wetland exhibiting frequent dry phases between 9800 and 9300 calendar years before present (cal. yr BP). There was a switch to a more positive water balance after 9300 cal. yr BP, and by 8000 cal. yr BP, there was a lake that persisted until 6100 cal. yr BP. The period between 6100 and 1000 cal. yr BP was much drier, and there is no evidence for a permanent lake during this period. The Little Llangothlin record provides evidence for a wet phase during the Early to Middle Holocene (9000–6000 cal. yr BP) from the boundary region between temperate and tropical influences in eastern Australia. We propose that generally enhanced circulation after 9000 cal. yr BP explains the pattern of increasing moisture at the site at this time. The later Holocene climate at the site is consistent with other sites in south east Australia with a switch to generally drier conditions after 6000 cal. yr BP.

Macrofossil

Ephemeral key

Before Present

10.1177/0959683614551218

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Citations (25)