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Two cores have currently been taken. One, collected in May 1992 at 5–10 metres (16–33 ft) depth, is 3 metres (10 ft) long and extends from 1708 to 1992. The second one was taken in
December 2017 at a depth of 5 metres (16 ft), and its 0.5 metres (2 ft) covers the period from 1835
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coral, which can live for hundreds of years and continue growing throughout this period. Cores taken from this coral have annual growth bands between 0.8 centimetres (0.31 in) and 1.6 centimetres (0.63 in) long. These annual bands preserve information about the water chemistry of the reef
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The reef is quite large compared to its neighbours, stretching 40 kilometres (25 mi) north to south. A continuous 15 kilometres (9 mi) reef barrier stretches down the
Eastern edge. Rising up from water over 1 kilometre (1 mi) deep, most of the reef lies at a depth of just 1–4 metres
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The main body is sometimes referred to as North
Flinders Reef, with South Flinders Reef being a smaller reef lying directly south of the main area. Dart Reef and Heralds Surprise are small reefs lying to the northwest and northeast respectively of the main reef.
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The remote location means
Flinders Reef and nearby reefs are poorly studied. The wildlife is distinct from that of the Great Barrier Reef, with these reefs likely acting as conduits for species dispersal between the Great Barrier Reef and the wider western
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genus, is much rarer. Concentrations of sponges can reach 1.2 kilograms (2.6 lb) per 1 square metre (11 sq ft), and they cover around 7.3 per cent of the reef flat. At least one of these species may be
93:. It is 120 kilometres (75 mi) from the Great Barrier Reef, and 250 kilometres (155 mi) northeast of the Australian coastline. The position of the reef is around 17°37'S, 148°31'E, with weather station
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isotopes indicate ocean acidity peaking in 2000. The environmental indicators in the cores from
Flinders Reef correlate with cores taken from multiple locations within the Great Barrier Reef.
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isotopes, information can be gained about surrounding ocean temperature, which began increasing in the 1850s, with this increase accelerating beginning in the 1970s.
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Pelejero, Carles; Calvo, Eva; McCulloch, Malcolm T.; Marshall, John F.; Gagan, Michael K.; Lough, Janice M.; Opdyke, Bradley N. (30 September 2005).
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Bridge, Tom C. L.; Beaman, Robin J.; Bongaerts, Pim; Muir, Paul R.; Ekins, Merrick; Sih, Tiffany (2019).
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and high rainfall. Water currents around the reef tend to originate from the southeast, propelled by
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Due to its isolation from local human influence, Flinders Reef is a candidate for the location of a
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510:"Continental shelf waves and their influence on the circulation around the Great Barrier Reef"
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Gazetteer of
Undersea Features: Names Approved by the United States Board on Geographic Names
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events. The prevailing wind is mostly westward, coming from 270°. The region sometimes sees
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405:"Productivity and abundance of large sponge populations on Flinders Reef flats, Coral Sea"
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591:"More than half of remote reefs in Coral Sea marine park suffered extreme bleaching"
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to 2017. Both cores show a rise of carbon-14 in the 1950s, related to the use of
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these sponges may extract over 50 per cent of their nutrition from sunlight.
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455:"Preindustrial to Modern Interdecadal Variability in Coral Reef pH"
541:"Roughness lengths and turbulence intensities for wind over water"
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Flinders Reef is one of a number of oceanic reefs rising from the
298:. In Loya, Yossi; Puglise, Kimberly A.; Bridge, Tom C.L. (eds.).
238:. The transition to the Anthropocene can be seen in samples of
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The reef flat areas of
Flinders Reef have large populations of
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379:(4 ed.). Defense Mapping Agency. 1990. p. I-43.
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Australian
Journal of Marine and Freshwater Research
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160:IUCN protected habitat or species management area
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133:(3–13 ft). Sand covers 25 per cent of the
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565:"Coral Sea Marine Park – Flinders Reefs"
112:. These currents form part of the wider
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355:. Anthropocene Curriculum. 11 May 2022
296:"The Great Barrier Reef and Coral Sea"
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181:, mostly consisting of four similar
89:to the south separating it from the
189:family, and one each of the genera
81:to the west separating it from the
589:Readfearn, Graham (9 April 2020).
403:Wilkinson, Clive R. (April 1987).
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508:Wolanski, E; Bennett, AF (1983).
207:. A fifth species, part of the
539:Holmes, J.D. (December 2017).
97:located at 17°44'S, 148°26'E.
22:Flinders Reef lies within the
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234:to mark the beginning of the
310:10.1007/978-3-319-92735-0_20
162:. One threat to the reef is
301:Mesophotic Coral Ecosystems
100:This area falls within the
24:Coral Sea Islands Territory
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670:Landforms of the Coral Sea
353:"Flinders Reef, Australia"
158:, and is designated as an
154:. The reef is part of the
245:at the time they formed.
618:3D map of Flinders Reefs
114:South Equatorial Current
479:10.1126/science.1113692
37:is an isolated oceanic
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61:the beginning of the
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421:1987CorRe...5..183W
226:Anthropocene marker
172:recreational diving
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641:17.619°S 148.464°E
429:10.1007/BF00300961
83:Great Barrier Reef
75:Queensland plateau
55:Great Barrier Reef
53:and the extensive
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665:Coral Sea Islands
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319:978-3-319-92735-0
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632:148°27′50″E
409:Coral Reefs
216:phototropic
210:Dictyonella
187:Thorectidae
110:trade winds
659:Categories
629:17°37′08″S
277:References
135:reef flats
85:, and the
39:coral reef
520:(1): 29.
495:129883047
328:181564042
263:strontium
128:Structure
102:Coral Sea
51:Australia
43:Coral Sea
600:6 August
574:6 August
487:16195458
437:41632439
122:cyclones
69:Location
467:Bibcode
459:Science
417:Bibcode
359:31 July
267:calcium
241:Porites
179:sponges
118:La Niña
41:in the
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265:, and
259:oxygen
201:, and
174:site.
568:(PDF)
544:(PDF)
491:S2CID
433:S2CID
324:S2CID
271:Boron
602:2022
576:2022
483:PMID
361:2022
314:ISBN
59:mark
522:doi
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