It is increasingly apparent that sea-level data (e.g. microfossil transfer functions, dated coral microatolls and direct observations from satellite and tidal gauges) vary temporally and spatially at regional to local scales, thus limiting our ability to model future sea-level rise for many regions. Understanding sea-level response at ‘far-field’ locations at regional scales is fundamental for formulating more relevant sea-level rise susceptibility models within these regions under future global change projections. Fossil corals and reefs in particular are valuable tools for reconstructing past sea levels and possible environmental phase shifts beyond the temporal constraints of instrumental records. This study used abundant surface geochronological data based on in situ subfossil corals and precise elevation surveys to determine previous sea level in Moreton Bay, eastern Australia, a far-field site. A total of 64 U-Th dates show that relative sea level was at least 1.1 m above modern lowest astronomical tide (LAT) from at least ~6600 cal. yr BP. Furthermore, a rapid synchronous demise in coral reef growth occurred in Moreton Bay ~5800 cal. yr BP, coinciding with reported reef hiatus periods in other areas around the Indo-Pacific region. Evaluating past reef growth patterns and phases allows for a better interpretation of anthropogenic forcing versus natural environmental/climatic cycles that effect reef formation and demise at all scales and may allow better prediction of reef response to future global change.
AbramNJMcgregorHVGaganMK. (2009) Oscillations in the southern extent of the Indo-Pacific warm pool during the mid-Holocene. Quaternary Science Reviews28: 2794–2803.
2.
AharonPChappellJ (1986) Oxygen isotopes, sea level changes and the temperature history of a coral reef environment in New Guinea over the last 105 years. Palaeogeography, Palaeoclimatology, Palaeoecology56: 337–379.
3.
AkumuCEPathiranaSBucherD. (2011) Examining the potential impacts of sea level rise on coastal wetlands in north-eastern NSW, Australia. Journal of Coastal Conservation15: 15–22.
4.
AllisonNWebsterAClagueD (2007) Paleoenvironmental records from fossil corals: The effects of submarine diagenesis on temperature and climate estimates. Geochimica et Cosmochimica Acta71: 4693–4703.
5.
BakerR (2001) Inter-tidal fixed indicators of former Holocene sea levels in Australia: A summary of sites and a review of methods and models. Quaternary International83–85: 257–273.
6.
BakerRHaworthRJ (2000) Smooth or oscillating late Holocene sea-level curve? Evidence from the palaeo-zoology of fixed biological indicators in east Australia and beyond. Marine Geology163: 367–386.
7.
BanerjeePK (2000) Holocene and Late Pleistocene relative sea level fluctuations along the east coast of India. Marine Geology167: 243–260.
8.
BindoffNLWillebrandJArtaleV. (2007) Observations: Oceanic climate change and sea level. In: SolomonSQinDManningM. (eds) Climate Change 2007: The Physical Science Basis (Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change). Cambridge: Cambridge University Press, pp. 387–429.
9.
BondGBonaniGKromerB. (2001) Persistent solar influence on North Atlantic climate during the Holocene. Science294: 2130–2136.
10.
BondGBonaniGShowersW. (1997) A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science278: 1257–1266.
11.
BrijkerJMJungSJAGanssenGM. (2007) ENSO related decadal scale climate variability from the Indo-Pacific warm pool. Earth and Planetary Science Letters253: 67–82.
12.
BrookeBRyanDPietschT. (2008) Influence of climate fluctuations and changes in catchment land use on Late Holocene and modern beach-ridge sedimentation on a tropical macrotidal coast: Keppel Bay, Queensland, Australia. Marine Geology251: 195–208.
13.
ChappellJ (1983) Evidence for smoothly falling sea-level relative to North Queensland, Australia, during the past 6,000 yr. Nature302: 406–408.
14.
ChengHEdwardsRLHoffJ. (2000) The half-lives of uranium-234 and thorium-230. Chemical Geology169: 17–33.
15.
ClarkTRZhaoJ-XFengY-X. (2012) Spatial variability of initial 230Th/232Th in modern Porites from the inshore region of the Great Barrier Reef. Geochimica et Cosmochimica Acta78: 99–118.
16.
ClementACSeagerRCaneMA (2000) Suppression of El Niño during the Mid-Holocene by changes in the Earth’s orbit. Paleoceanography15: 731–737.
17.
CobbKMCharlesCDChengH. (2003) U/Th-dating living and young fossil corals from the central tropical Pacific. Earth and Planetary Science Letters210: 91–103.
18.
CollinsLBJian-XinZFreemanH (2006) A high-precision record of mid-late Holocene sea-level events from emergent coral pavements in the Houtman Abrolhos Islands, southwest Australia. Quaternary International145–146: 78–85.
19.
ComptonJ (2001) Holocene sea-level fluctuations inferred from the evolution of depositional environments of the southern Langebaan Lagoon salt marsh, South Africa. The Holocene11: 395–405.
20.
ComptonJS (2006) The Mid-Holocene sea-level highstand at Bogenfels Pan on the southwest coast of Namibia. Quaternary Research66: 303–310.
21.
CrowleyGMGaganMK (1995) Holocene evolution of coastal wetlands in wet-tropical northeastern Australia. The Holocene5: 385–399.
22.
DaviesPKinseyDW (1977) Holocene reef growth – One Tree Island, Great Barrier Reef. Marine Geology24: 1–11.
23.
De DeckkerPYokoyamaY (2009) Micropalaeontological evidence for Late Quaternary sea-level changes in Bonaparte Gulf, Australia. Global and Planetary Change66: 85–92.
24.
DondersTHWagnerFVisscherH (2006) Late Pleistocene and Holocene subtropical vegetation dynamics recorded in perched lake deposits on Fraser Island, Queensland, Australia. Palaeogeography, Palaeoclimatology, Palaeoecology241: 417–439.
25.
EdwardsR (2007) Sea levels: Resolution and uncertainty. Progress in Physical Geography31: 621–632.
26.
EdwardsR (2008) Sea levels: Science and society. Progress in Physical Geography32: 557–574.
EsatTMYokoyamaY (2010) Coupled uranium isotope and sea-level variations in the oceans. Geochimica et Cosmochimica Acta74: 7008–7020.
29.
EvansKGStephensAWShortenGG (1992) Quaternary sequence stratigraphy of the Brisbane River delta, Moreton Bay, Australia. Marine Geology107: 61–68, IN11–IN12, 69–70, IN13–IN14, 71–79.
30.
FellegaraIHarrisonPL (2008) Status of the subtropical scleractinian coral communities in the turbid environment of Moreton Bay, southeast Queensland. In: DaviePJFPhillipsJA (eds) Proceedings of the Thirteenth International Marine Biological Workshop: The Marine Fauna and Flora of Moreton Bay, Queensland (Memoirs of the Queensland Museum – Nature). Brisbane: Queensland Museum, pp. 277–291.
31.
FloodPG (1978) The significance of two contrasting sedimentary environments (the Fringing Coral Reef and the Tidal Mud Flat) presently in juxtaposition along the southwestern shore of Moreton Bay, Queensland. Papers, Department of Geology, University of Queensland8: 44–63.
32.
FloodPG (1984) A review of Holocene sea level data, southeastern Queensland. In: ColemanRJCovacevichJ (eds) Focus on Stradbroke: New Information on North Stradbroke Island and Surrounding Areas, 1974–1984 (Papers Prepared for the Royal Society of Queensland Symposium). Brisbane: Boolarong Publications, pp. 127–131.
33.
GehrelsWRRoeHMCharmanDJ (2001) Foraminifera, testate amoebae and diatoms as sea-level indicators in UK saltmarshes: A quantitative multiproxy approach. Journal of Quaternary Science16: 201–220.
34.
GillEHopleyD (1972) Holocene sea levels in eastern Australia – A discussion. Marine Geology12: 223–233.
35.
GuinotteJMBuddemeierRWKleypasJA (2003) Future coral reef habitat marginality: Temporal and spatial effects of climate change in the Pacific basin. Coral Reefs22: 551–558.
36.
HamanakaNKanHYokoyamaY. (2012) Disturbances with hiatuses in high-latitude coral reef growth during the Holocene: Correlation with millennial-scale global climate change. Global and Planetary Change 80–81: 21–35.
37.
HaugGHHughenKASigmanDM. (2001) Southward migration of the intertropical convergence zone through the Holocene. Science293: 1304–1308.
38.
HaworthRJFloodPGBakerRGV (2002) Predicted and observed Holocene sea-levels on the Australian coast: What do they indicate about hydro-isostatic models in far-field sites?Journal of Quaternary Science17: 581–591.
39.
HekelHWardWTJonesM (1979) Geological development of northern Moreton Bay. In: BaileyAStevensNC (eds) Northern Moreton Bay Symposium (Proceedings of a Symposium Held at the Abel Smith Lecture Theatre, University of Queensland, September 23–24). Brisbane: Royal Society of Queensland, pp. 7–18.
40.
HendersonGM (2002) Seawater (234U/238U) during the last 800 thousand years. Earth and Planetary Science Letters199: 97–110.
41.
HendersonGM (2005) Coral clues to rapid sea-level change. Science308: 361–362.
42.
HenneckeWG (2004) GIS modelling of sea-level rise induced shoreline changes inside coastal Re-Rntrants – Two examples from southeastern Australia. Natural Hazards31: 253–276.
43.
HongoCKayanneH (2009) Holocene coral reef development under windward and leeward locations at Ishigaki Island, Ryukyu Islands, Japan. Sedimentary Geology214: 62–73.
44.
HongoCKayanneH (2010) Holocene sea-level record from corals: Reliability of paleodepth indicators at Ishigaki Island, Ryukyu Islands, Japan. Palaeogeography, Palaeoclimatology, Palaeoecology287: 143–151.
45.
HopleyDGillE (1972) Holocene sea levels in eastern Australia – A discussion. Marine Geology12: 223–233.
46.
HopleyDSmithersS (2010) Encyclopedia of the World’s Coastal Landforms. Dordrecht: Springer.
47.
HughesTPBairdAHDinsdaleEA. (2002) Detecting regional variation using meta-analysis and large-scale sampling: Latitudinal patterns in recruitment. Ecology83: 436–451.
48.
HunterJ (2010) Estimating sea-level extremes under conditions of uncertain sea-level rise. Climatic Change99: 331–350.
49.
Intergovernmental Panel on Climate Change (IPCC) (2007) Climate Change 2007: Impacts, Adaptation and Vulnerability (Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change). Cambridge: Cambridge University Press.
50.
JohnsonPRNeilDT (1998) The corals of Moreton Bay: Living with extremes. In: HallNJTibbettsIRDennisonW (eds) Moreton Bay and Catchment. Brisbane: School of Marine Science, University of Queensland, pp. 503–524.
51.
JonesMHekelHSearleDE (1978) Late Quaternary sedimentation in Moreton Bay. Papers, Department of Geology, University of Queensland, 8: 6–17.
52.
JuckesMNAllenMRBriffaKR. (2007) Millennial temperature reconstruction intercomparison and evaluation. Climate of the Past3: 591–609.
53.
KempJRadkeLCOlleyJ. (2012) Holocene lake salinity changes in the Wimmera, southeastern Australia, provide evidence for millennial-scale climate variability. Quaternary Research77: 65–76.
54.
KroekerKJMicheliFGambiMC. (2011) Divergent ecosystem responses within a benthic marine community to ocean acidification. PNAS108: 14515–14520.
55.
LambeckKNakadaM (1990) Late Pleistocene and Holocene sea-level change along the Australian coast. Palaeogeography, Palaeoclimatology, Palaeoecology (Global and Planetary Change Section) 89: 143–176.
56.
LambeckKWoodroffeCDAntonioliF. (2010) Paleoenvironmental records, geophysical modelling and reconstruction of sea-level trends and variability on centennial and longer timescales. In: ChurchJWoodworthTAarupWS (eds) Understanding Sea-Level Rise and Variability. Hoboken, NJ: Blackwell Publishing Ltd, pp. 61–121.
57.
LangSCMcClureSTGrosserM. (1998) Sedimentation and coastal evolution, northern Moreton Bay. In: TibbetsIRHallNJDennisonWC (eds) Moreton Bay and Catchment. Brisbane: School of Marine Science, The University of Queensland, pp. 81–92.
58.
LewisSESlossCRMurray-WallaceCV. (2013) Post-glacial sea-level changes around the Australian margin: A review. Quaternary Science Reviews74: 115–138.
59.
LewisSEWustRAJWebsterJM. (2008) Mid-late Holocene sea-level variability in eastern Australia. Terra Nova20: 74–81.
60.
LiuZHarrisonSPKutzbachJ. (2004) Global monsoons in the mid-Holocene and oceanic feedback. Climate Dynamics22: 157–182.
61.
LjungqvistFC (2011) The spatio-temporal pattern of the Mid-Holocene thermal maximum. Geografie116: 91–110.
62.
LoehleCSingerSF (2010) Holocene temperature records show millennial-scale periodicity. Canadian Journal of Earth Sciences47: 1327–1336.
63.
LongA (2001) Mid-Holocene sea-level change and coastal evolution. Progress in Physical Geography25: 399–408.
64.
LovellE (1975) Evidence for a higher sea level in Moreton Bay. Marine Geology18: 87–94.
65.
LudwigKR (2003) Isoplot/Ex, version 3: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publications.
66.
LyboltMNeilDTZhaoJ. (2011) Instability in a marginal coral reef: The shift from natural variability to a human-dominated seascape. Frontiers in Ecology and the Environment9: 154–160.
67.
McCullochM (2000) The coral record of last interglacial sea levels and sea surface temperatures. Chemical Geology169: 107–129.
68.
McGowanHAPetherickLMKamberBS (2008) Aeolian sedimentation and climate variability during the late Quaternary in southeast Queensland, Australia. Palaeogeography, Palaeoclimatology, Palaeoecology265: 171–181.
69.
McGregorHGaganMK (2003) Diagenesis and geochemistry of Porites corals from Papua New Guinea: Implications for paleoclimate reconstruction. Geochimica et Cosmochimica Acta67: 2147–2156.
70.
McGregorHVGaganMK (2004) Western Pacific coral δ18O records of anomalous Holocene variability in the El-Nino-Southern Oscillation. Geophysical Research Letters31: 1–4.
71.
MannMERutherfordSWahlE. (2005) Testing the fidelity of methods used in proxy-based reconstructions of past climate. Journal of Climate18: 4097.
72.
MarxSKKamberBSMcgowanHA. (2009) Detailed history of Holocene climate variability in Australia from dust records in peat cores. Geochimica et Cosmochimica Acta73: A843.
MeyssignacBCazenaveA (2012) Sea level: A review of present-day and recent-past changes and variability. Journal of Geodynamics58: 96–109.
77.
MohtadiMOppoDWSteinkeS. (2011) Glacial to Holocene swings of the Australian-Indonesian monsoon. Nature Geoscience4: 540–544.
78.
MorosMDe DeckkerPJansenE. (2009) Holocene climate variability in the Southern Ocean recorded in a deep-sea sediment core off South Australia. Quaternary Science Reviews28: 1932–1940.
79.
MossPTTibbyJPetherickL. (2013) Late Quaternary vegetation history of North Stradbroke Island, Queensland, eastern Australia. Quaternary Science Reviews74: 257–272.
80.
NarayanYR (2011) Benthic foraminifera as Holocene to Recent indicators in marginal marine environments: Modern distribution and the palaeoecological response to environmental changes in Moreton Bay, southeastern Queensland. PhD Thesis, The University of Queensland.
81.
NeumannACMacintyreIG (1985) Reef response to sea level rise: Keep-up, catch up or give-up. In: GabrieCToffartJLSalvatB (eds) Proceedings of the 5th International Coral Reef Congress. Tahiti: Antenne Museum–EPHE, pp. 105–110.
82.
NguyenAD (2012) Climatic and environmental reconstruction based on Holocene coral reefs on central Vietnamese coast, western South China Sea. PhD Thesis, The University of Queensland, 241 pp.
83.
NothdurftLDWebbGE (2009) Earliest diagenesis in scleractinian coral skeletons: Implications for paleoclimate-sensitive geochemical archives. Facies55: 161–201.
84.
NothdurftLDWebbGEBostromT. (2007) Calcite-filled borings in the most recently deposited skeleton in live-collected Porites (Scleractinia): Implications for trace element archives. Geochimica et Cosmochimica Acta71: 5423–5438.
85.
PantusFDennisonW (2005) Quantifying and evaluating ecosystem health: A case study from Moreton Bay, Australia. Environmental Management36: 757–771.
86.
PartinJWCobbKMAdkinsJF. (2007) Millennial-scale trends in west Pacific warm pool hydrology since the Last Glacial Maximum. Nature449: 452–455.
87.
PattiaratchiCBHarrisPT (2002) Hydrodynamic and sand-transport controls on sandbank formation: An example from Moreton Bay, eastern Australia. Marine & Freshwater Research53: 1101–1113.
88.
PerryCSmithersS (2011) Cycles of coral reef ‘turn-on’, rapid growth and ‘turn-off’ over the past 8500 years: A context for understanding modern ecological states and trajectories. Global Change Biology17: 76–86.
89.
PetherickLBostockHCohenTJ. (2013) Climatic records over the past 30 ka from temperate Australia – Asynthesis from the Oz-INTIMATE workgroup. Quaternary Science Reviews74: 58–77.
90.
PredaMCoxME (2000) Sediment-water interaction, acidity and other water quality parameters in a subtropical setting, Pimpama River, southeast Queensland. Environmental Geology39: 319–329.
91.
Ribaud-LaurentiAMontaggioniLHamelinB. (2001) Diagenesis and its impact on Sr/Ca ratio in Holocene Acropora corals. International Journal of Earth Sciences90: 438–451.
92.
RobertsLGHarriottVJ (2003) Can environmental records be extracted from coral skeletons from Moreton Bay, Australia, a subtropical, turbid environment?Coral Reefs22: 517–522.
93.
RoffGClarkTRReymondCE. (2013) Palaeoecological evidence of a historical collapse of corals at Pelorus Island, inshore Great Barrier Reef, following European settlement. Proceedings of the Royal Society B: Biological Sciences280: 1750.
94.
ScoffinTPTissierMDA (1998) Late Holocene sea level and reef-flat progradation, Phuket, South Thailand. Coral Reefs17: 273–276.
95.
ScoffinTPStoddartDRRosenBR (1978) The nature and significance of microatolls. Philosophical Transactions of the Royal Society of London, Series B284: 99–122.
96.
ShenC-CFanT-YMeltznerAJ. (2008) Variation of initial 230Th/232Th and limits of high precision U–Th dating of shallow-water corals. Geochimica et Cosmochimica Acta72: 4201–4223.
97.
ShulmeisterJLeesBG (1995) Pollen evidence from tropical Australia for the onset of an ENSO-dominated climate at c. 4000 BP. The Holocene5: 10–18.
98.
SlossCRMurray-WallaceCVJonesBG (2007) Holocene sea-level change on the southeast coast of Australia: A review. The Holocene17: 999–1014.
99.
SmithDEHarrisonSFirthCR. (2011) The early Holocene sea level rise. Quaternary Science Reviews30: 1846–1860.
100.
SmithersSGWoodroffeCD (2000) Microatolls as sea-level indicators on a mid-ocean atoll. Marine Geology168: 61–78.
101.
SmithersSGHopleyDParnellKE (2006) Fringing and nearshore coral reefs of the Great Barrier Reef: Episodic Holocene development and future prospects. Journal of Coastal Research22: 175–187.
102.
StoddartDRScoffinTP (1979) Microatolls: Review of form, origin and terminology. Atoll Research Bulletin224: 1–17.
103.
SwitzerASlossCRJonesBG. (2010) Geomorphic evidence for mid-late Holocene higher sea level from southeastern Australia. Quaternary International221: 13–22.
104.
TudhopeAWChilcottCPMcCullochMT. (2001) Variability in the El Niño-Southern Oscillation through a glacial-interglacial cycle. Science (New York, N.Y.)291: 1511–1517.
105.
UlmSPetcheyFRossA (2009) Marine reservoir corrections for Moreton Bay, Australia. Archaeology in Oceania44: 160–168.
106.
VeronJEN (1993) Corals of Australia and the Indo-Pacific. Sydney: Angus & Robertson.
107.
WallaceCCFellegaraIMuirP (2009) The scleractinian corals of Moreton Bay, eastern Australia: High latitude, marginal assemblages with increasing species richness. In: DaviePJFPhillipsJA (eds) Proceedings of the Thirteenth International Marine Biological Workshop: The Marine Fauna and Flora of Moreton Bay, Queensland (Memoirs of the Queensland Museum – Nature). Brisbane: Queensland Museum, pp. 1–113.
108.
WangBWangY (1999) Dynamics of the ITCZ-Equatorial Cold Tongue Complex and causes of the latitudinal climate asymmetry. Journal of Climate12: 1830–1847.
109.
WangYJChengHEdwardsRL. (2005) The Holocene Asian monsoon: Links to solar changes and North Atlantic climate. Science308(5723): 854–857.
110.
WannerHKaplanJOKüttelM. (2008) Mid- to Late Holocene climate change: An overview. Quaternary Science Reviews27: 1791–1828.
111.
WardWTHackerJ (2006) Brisbane Airport: An alluvial landscape veiled by marine sediments. Australian Journal of Earth Sciences53: 1001–1012.
112.
WebbGENothdurftLDKamberBS. (2009) Rare earth element geochemistry of scleractinian coral skeleton during meteoric diagenesis: A sequence through neomorphism of aragonite to calcite. Sedimentology56: 1433–1463.
113.
WellsJW (1955) Recent and Subfossil Corals of Moreton Bay, Queensland. Brisbane: Queensland University Press.
114.
WoodroffeCDMurray-WallaceCV (2012) Sea-level rise and coastal change: The past as a guide to the future. Quaternary Science Reviews54: 4–11.
115.
WoodroffeSA (2009) Testing models of mid to late Holocene sea-level change, North Queensland, Australia. Quaternary Science Reviews28: 2474–2488.
116.
YokoyamaYEsatTM (2011) Global climate and sea level enduring variability and rapid fluctuations over the past 150,000 years. Oceanography24: 54–69.
117.
YokoyamaYPurcellAMarshallJF. (2006) Sea-level during the early deglaciation period in the Great Barrier Reef, Australia. Global and Planetary Change53: 147–153.
118.
YuKFChenTG (2009) Beach sediments from northern South China Sea suggest high and oscillating sea level during the late Holocene. Earth Science Frontiers16: 138–145.
119.
YuKFZhaoJX (2010) U-series dates of Great Barrier Reef corals suggest at least+0.7 m sea level ~ 7000 years ago. The Holocene20: 161–168.
120.
YuK-FZhaoJ-XDoneT. (2009) Microatoll record for large century-scale sea-level fluctuations in the mid-Holocene. Quaternary Research71: 354–360.
121.
ZhaoJXYuKF (2002) Timing of Holocene sea-level highstands by mass spectrometric U-series ages of a coral reef from Leizhou Peninsula, South China Sea. Chinese Science Bulletin47: 348–352.
122.
ZhaoJXYuKF (2007) Millennial, century and decadal scale oscillations of Holocene sea level recorded in a coral reef in the northern South China Sea. Quaternary International167–168(Suppl. 1): 473.
123.
ZhouHYZhaoJXWangQ. (2011) Speleothem-derived Asian summer monsoon variations in Central China during 54–46 ka. Journal of Quaternary Science26: 781–790.
