Knowledge (XXG)

Flinders Reef (Coral Sea)

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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 273:
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).
317: 669: 159: 352: 674: 564: 57:. Due to its remote location, it remains poorly studied. However, this isolation has also made it a potential site to 23: 664: 113: 253:, which declines after 1975. They also preserve changes in carbon isotopes which are caused by the burning of 294:
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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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
105: 405:"Productivity and abundance of large sponge populations on Flinders Reef flats, Coral Sea" 203: 191: 167: 470: 420: 404: 250: 182: 163: 116:. This drives changes in pH in the reef water, while annual pH changes are affected by 18: 454: 658: 494: 327: 219: 151: 46: 591:"More than half of remote reefs in Coral Sea marine park suffered extreme bleaching" 436: 235: 215: 62: 309: 249:
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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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 177:
The reef flat areas of Flinders Reef have large populations of
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Australian Journal of Marine and Freshwater Research
559: 557: 160:IUCN protected habitat or species management area 548:9th Asia-Pacific Conference on Wind Engineering 398: 396: 394: 392: 390: 388: 386: 133:(3–13 ft). Sand covers 25 per cent of the 448: 446: 8: 289: 287: 285: 232:Global Boundary Stratotype Section and Point 77:. It lies near the southwest edge, with the 347: 345: 343: 341: 339: 337: 218:, and through partnership with symbiotic 565:"Coral Sea Marine Park – Flinders Reefs" 112:. These currents form part of the wider 17: 281: 355:. Anthropocene Curriculum. 11 May 2022 296:"The Great Barrier Reef and Coral Sea" 7: 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). 14: 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 1: 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 691: 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 185:species: one from the 27: 257:. Through changes in 156:Coral Sea Marine Park 61:the beginning of the 21: 637: /  471:2005Sci...309.2204P 465:(5744): 2204–2207. 421:1987CorRe...5..183W 226:Anthropocene marker 172:recreational diving 166:, which has caused 675:Reefs of Australia 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 49:. It lies east of 28: 665:Coral Sea Islands 526:10.1071/MF9830023 319:978-3-319-92735-0 87:Townsville trough 79:Queensland trough 682: 652: 651: 649: 648: 647: 646:-17.619; 148.464 642: 638: 635: 634: 633: 630: 606: 605: 603: 601: 586: 580: 579: 577: 575: 569: 561: 552: 551: 545: 536: 530: 529: 505: 499: 498: 450: 441: 440: 400: 381: 380: 371: 365: 364: 362: 360: 349: 332: 331: 291: 170:. The area is a 106:tropical climate 690: 689: 685: 684: 683: 681: 680: 679: 655: 654: 645: 643: 639: 636: 631: 628: 626: 624: 623: 614: 609: 599: 597: 588: 587: 583: 573: 571: 567: 563: 562: 555: 543: 538: 537: 533: 507: 506: 502: 452: 451: 444: 402: 401: 384: 373: 372: 368: 358: 356: 351: 350: 335: 320: 293: 292: 283: 279: 251:nuclear weapons 228: 204:Carteriospongia 192:Carteriospongia 168:coral bleaching 147: 130: 71: 45:of the western 12: 11: 5: 688: 686: 678: 677: 672: 667: 657: 656: 621: 620: 613: 612:External links 610: 608: 607: 581: 553: 531: 500: 442: 415:(4): 183–188. 382: 366: 333: 318: 280: 278: 275: 227: 224: 183:Dictyoceratida 164:climate change 146: 143: 129: 126: 104:, which has a 91:Marion plateau 70: 67: 35:Flinders Reefs 13: 10: 9: 6: 4: 3: 2: 687: 676: 673: 671: 668: 666: 663: 662: 660: 653: 650: 619: 616: 615: 611: 596: 592: 585: 582: 566: 560: 558: 554: 549: 542: 535: 532: 527: 523: 519: 515: 511: 504: 501: 496: 492: 488: 484: 480: 476: 472: 468: 464: 460: 456: 449: 447: 443: 438: 434: 430: 426: 422: 418: 414: 410: 406: 399: 397: 395: 393: 391: 389: 387: 383: 378: 377: 370: 367: 354: 348: 346: 344: 342: 340: 338: 334: 329: 325: 321: 315: 311: 307: 303: 302: 297: 290: 288: 286: 282: 276: 274: 272: 268: 264: 260: 256: 252: 246: 243: 242: 237: 233: 225: 223: 221: 220:cyanobacteria 217: 212: 211: 206: 205: 200: 199: 198:Phyllospongia 194: 193: 188: 184: 180: 175: 173: 169: 165: 161: 157: 153: 152:Pacific Ocean 144: 142: 138: 136: 127: 125: 123: 119: 115: 111: 107: 103: 98: 96: 92: 88: 84: 80: 76: 68: 66: 64: 60: 56: 52: 48: 47:Pacific Ocean 44: 40: 36: 32: 31:Flinders Reef 25: 20: 16: 622: 598:. Retrieved 595:The Guardian 594: 584: 572:. Retrieved 547: 534: 517: 513: 503: 462: 458: 412: 408: 375: 369: 357:. Retrieved 304:. Springer. 300: 255:fossil fuels 247: 239: 236:Anthropocene 229: 208: 202: 196: 190: 176: 148: 145:Biodiversity 139: 131: 99: 72: 63:Anthropocene 34: 30: 29: 15: 644: / 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 493:  485:  435:  326:  316:  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 475:doi 463:309 425:doi 306:doi 95:Cay 33:or 661:: 593:. 556:^ 546:. 518:34 516:. 512:. 489:. 481:. 473:. 461:. 457:. 445:^ 431:. 423:. 411:. 407:. 385:^ 336:^ 322:. 312:. 284:^ 261:, 195:, 137:. 124:. 65:. 604:. 578:. 550:. 528:. 524:: 497:. 477:: 469:: 439:. 427:: 419:: 413:5 363:. 330:. 308:: 26:.

Index

Map showing the Coral Sea Islands Territory off the Northeast coast of Australia
Coral Sea Islands Territory
coral reef
Coral Sea
Pacific Ocean
Australia
Great Barrier Reef
mark
Anthropocene
Queensland plateau
Queensland trough
Great Barrier Reef
Townsville trough
Marion plateau
Cay
Coral Sea
tropical climate
trade winds
South Equatorial Current
La Niña
cyclones
reef flats
Pacific Ocean
Coral Sea Marine Park
IUCN protected habitat or species management area
climate change
coral bleaching
recreational diving
sponges
Dictyoceratida

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