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Journal articles on the topic 'Ningaloo'

Author: Grafiati

Published: 4 June 2021

Last updated: 2 February 2022

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1

Morton, Brian. "Ningaloo." Marine Pollution Bulletin 46, no. 10 (October 2003): 1213–14. http://dx.doi.org/10.1016/j.marpolbul.2003.08.011.

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2

Zhang, Lei, Weiqing Han, Yuanlong Li, and Toshiaki Shinoda. "Mechanisms for Generation and Development of the Ningaloo Niño." Journal of Climate 31, no. 22 (November 2018): 9239–59. http://dx.doi.org/10.1175/jcli-d-18-0175.1.

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Generation and development mechanisms of the Ningaloo Niño are investigated using ocean and atmospheric general circulation model experiments. Consistent with previous studies, northerly wind anomalies off the West Australian coast are critical in generating warm sea surface temperature (SST) anomalies of the Ningaloo Niño, which induce SST warming through reduced turbulent heat loss toward the atmosphere (by decreasing surface wind speed), enhanced Leeuwin Current heat transport, and weakened coastal upwelling. Our results further reveal that northerly wind anomalies suppress the cold dry air

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3

Beckley, Lynnath E., and Amanda T. Lombard. "A systematic evaluation of the incremental protection of broad-scale habitats at Ningaloo Reef, Western Australia." Marine and Freshwater Research 63, no. 1 (2012): 17. http://dx.doi.org/10.1071/mf11074.

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Incremental increases to marine conservation areas in response to changing goals, policy, threats or new information are common practice worldwide. Ningaloo Reef, in north-western Australia, is protected by the Ningaloo Marine Park (state waters), which was expanded incrementally in 2004 so that 34% of the park now comprises ‘no-take’ sanctuary zones. To test the hypothesis that all habitats (benthic cover types) at Ningaloo are actually protected at this 34% level, a systematic conservation planning exercise was conducted using existing broad-scale habitat data (as a surrogate for marine biod

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4

Norman, Bradley M., Samantha Reynolds, and David L. Morgan. "Does the whale shark aggregate along the Western Australian coastline beyond Ningaloo Reef?" Pacific Conservation Biology 22, no. 1 (2016): 72. http://dx.doi.org/10.1071/pc15045.

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Whale sharks (Rhincodon typus) seasonally aggregate at Western Australia’s Ningaloo Reef in the austral autumn and winter, but their occurrence beyond this region during spring and summer remains elusive. The aggregation at Ningaloo Reef coincides with a pulse of productivity following mass coral spawning in early autumn, with the population during this period dominated by juveniles that amass for feeding purposes. To investigate their movement patterns beyond Ningaloo Reef, whale sharks were fitted with SPOT (n = 13) or SPLASH (n = 1) tags between April and September (2010–14). Tagged whale s

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5

Jackson, George D., Mark G. Meekan, Simon Wotherspoon, and Christine H. Jackson. "Distributions of young cephalopods in the tropical waters of Western Australia over two consecutive summers." ICES Journal of Marine Science 65, no. 2 (January 15, 2008): 140–47. http://dx.doi.org/10.1093/icesjms/fsm186.

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Abstract Jackson, G. D., Meekan, M. G., Wotherspoon, S., and Jackson, C. H. 2008. Distributions of young cephalopods in the tropical waters of Western Australia over two consecutive summers. – ICES Journal of Marine Science, 65: 140–147. Cephalopod paralarvae and juveniles were sampled with light traps deployed at the surface and deeper in the southern NW Shelf and on Ningaloo Reef off Western Australia during two consecutive summers. One cross shelf transect (Exmouth) was sampled in the late spring and summers of 1997/1998 (summer 1) and 1998/1999 (summer 2), and a second cross shelf transect

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6

Kataoka, Takahito, Tomoki Tozuka, Swadhin Behera, and Toshio Yamagata. "On the Ningaloo Niño/Niña." Climate Dynamics 43, no. 5-6 (October 15, 2013): 1463–82. http://dx.doi.org/10.1007/s00382-013-1961-z.

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7

Preen, A. R., H. Marsh, I. R. Lawler, R. I. T. Prince, and R. Shepherd. "Distribution and Abundance of Dugongs, Turtles, Dolphins and other Megafauna in Shark Bay, Ningaloo Reef and Exmouth Gulf, Western Australia." Wildlife Research 24, no. 2 (1997): 185. http://dx.doi.org/10.1071/wr95078.

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Strip-transect aerial surveys of Shark Bay, Ningaloo Reef and Exmouth Gulf were conducted during the winters of 1989 and 1994. These surveys were designed primarily to estimate the abundance and distribution of dugongs, although they also allowed sea turtles and dolphins, and, to a lesser extent, whales, manta rays and whale sharks to be surveyed. Shark Bay contains a large population of dugongs that is of international significance. Estimates of approximately 10000 dugongs resulted from both surveys. The density of dugongs is the highest recorded in Australia and the Middle East, where these

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8

Guo, Yaru, Yuanlong Li, Fan Wang, Yuntao Wei, and Zengrui Rong. "Processes Controlling Sea Surface Temperature Variability of Ningaloo Niño." Journal of Climate 33, no. 10 (May 15, 2020): 4369–89. http://dx.doi.org/10.1175/jcli-d-19-0698.1.

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AbstractA high-resolution (3–8 km) regional oceanic general circulation model is utilized to understand the sea surface temperature (SST) variability of Ningaloo Niño in the southeast Indian Ocean (SEIO). The model reproduces eight Ningaloo Niño events with good fidelity and reveals complicated spatial structures. Mesoscale noises are seen in the warming signature and confirmed by satellite microwave SST data. Model experiments are carried out to quantitatively evaluate the effects of key processes. The results reveal that the surface turbulent heat flux (primarily latent heat flux) is the mos

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9

Gales, Nick, Robert D. McCauley, Janet Lanyon, and Dave Holley. "Change in abundance of dugongs in Shark Bay, Ningaloo and Exmouth Gulf, Western Australia: evidence for large-scale migration." Wildlife Research 31, no. 3 (2004): 283. http://dx.doi.org/10.1071/wr02073.

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The third in a series of five-yearly aerial surveys for dugongs in Shark Bay, Ningaloo Reef and Exmouth Gulf was conducted in July 1999. The first two surveys provided evidence of an apparently stable population of dugongs, with ~1000 animals in each of Exmouth Gulf and Ningaloo Reef, and 10 000 in Shark Bay. We report estimates of less than 200 for each of Exmouth Gulf and Ningaloo Reef and ~14 000 for Shark Bay. This is an apparent overall increase in the dugong population over this whole region, but with a distributional shift of animals to the south. The most plausible hypothesis to accoun

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10

Marshall, Andrew G., Harry H. Hendon, Ming Feng, and Andreas Schiller. "Initiation and amplification of the Ningaloo Niño." Climate Dynamics 45, no. 9-10 (January 22, 2015): 2367–85. http://dx.doi.org/10.1007/s00382-015-2477-5.

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11

Kido, Shoichiro, Takahito Kataoka, and Tomoki Tozuka. "Ningaloo Niño simulated in the CMIP5 models." Climate Dynamics 47, no. 5-6 (November 21, 2015): 1469–84. http://dx.doi.org/10.1007/s00382-015-2913-6.

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12

Lydia Schönberg, Christine Hanna. "The Sponge Gardens of Ningaloo Reef, Western Australia." Open Marine Biology Journal 4, no. 1 (October 12, 2010): 3–11. http://dx.doi.org/10.2174/1874450801004010003.

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13

Davis, Derrin. "Whale Shark Tourism in Ningaloo Marine Park, Australia." Anthrozoös 11, no. 1 (March 1998): 5–11. http://dx.doi.org/10.2752/089279398787000850.

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14

O'Shea, Owen R., Michele Thums, Mike van Keulen, and Mark Meekan. "Bioturbation by stingrays at Ningaloo Reef, Western Australia." Marine and Freshwater Research 63, no. 3 (2012): 189. http://dx.doi.org/10.1071/mf11180.

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Stingrays are an important part of the biomass of the fishes in shallow coastal ecosystems, particularly in inter-reefal areas. In these habitats, they are considered keystone species – modifying physical and biological habitats through their foraging and predation. Here, we quantify the effects of bioturbation by rays on sand flats of Ningaloo Reef lagoon in Western Australia. We measured the daily length, breadth and depth of 108 feeding pits over three 7‐day periods, created by stingrays (Pastinachus atrus, Himantura spp. Taeniura lymma and Urogymnus asperrimus) in Mangrove Bay. Additionall

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15

Kataoka, Takahito, Tomoki Tozuka, and Toshio Yamagata. "Generation and Decay Mechanisms of Ningaloo Niño/Niña." Journal of Geophysical Research: Oceans 122, no. 11 (November 2017): 8913–32. http://dx.doi.org/10.1002/2017jc012966.

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16

Ceh, Janja, Mike Van Keulen, and David G. Bourne. "Coral-associated bacterial communities on Ningaloo Reef, Western Australia." FEMS Microbiology Ecology 75, no. 1 (November 2, 2010): 134–44. http://dx.doi.org/10.1111/j.1574-6941.2010.00986.x.

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17

van Keulen, Mike. "Multiple climate impacts on seagrass dynamics: Amphibolis antarctica patches at Ningaloo Reef, Western Australia." Pacific Conservation Biology 25, no. 2 (2019): 211. http://dx.doi.org/10.1071/pc18050.

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The impacts of tropical cyclones combined with a marine heatwave are reported for a seagrass community at Ningaloo Reef, Western Australia. A community of 9.5ha of Amphibolis antarctica was lost following a combination of cyclone-induced burial and a marine heatwave. No new seedlings have been observed since the loss; recruitment of seedlings may be impeded by local ocean circulation.

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18

Sleeman, Jai C., Mark G. Meekan, Steven G. Wilson, Curt K. S. Jenner, Micheline N. Jenner, Guy S. Boggs, Craig C. Steinberg, and Corey J. A. Bradshaw. "Biophysical correlates of relative abundances of marine megafauna at Ningaloo Reef, Western Australia." Marine and Freshwater Research 58, no. 7 (2007): 608. http://dx.doi.org/10.1071/mf06213.

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Changes in the relative abundance of marine megafauna (whales, dolphins, sharks, turtles, manta rays, dugongs) from aerial survey sightings in the waters adjacent to Ningaloo Reef between June 2000 and April 2002 are described. Generalised linear models were used to explore relationships between different trophic guilds of animals (based on animal sighting biomass estimates) and biophysical features of the oceanscape that were likely to indicate foraging habitats (regions of primary/secondary production) including sea surface temperature (SST), SST gradient, chlorophyll-a (Chl-a), bathymetry (

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19

Przeslawski, Rachel, Matthew A. McArthur, and Tara J. Anderson. "Infaunal biodiversity patterns from Carnarvon Shelf (Ningaloo Reef), Western Australia." Marine and Freshwater Research 64, no. 6 (2013): 573. http://dx.doi.org/10.1071/mf12240.

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Infauna are important in many ecological processes but have been rarely considered in biodiversity assessments of coral reefs and surrounding areas. We surveyed infaunal assemblages and associated environmental factors (depth, seabed reflectance, sediment characteristics) in three areas (Mandu, Point Cloates, Gnaraloo) along the Carnarvon Shelf, Western Australia. This region supports Ningaloo Reef, a relatively pristine coral reef protected by the Ningaloo Marine Park and a Commonwealth marine reserve. Macrofauna were sampled with a Smith-McIntyre grab and sieved through 500 µm. A total of 42

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20

Mau, Roland. "Managing for Conservation and Recreation: The Ningaloo Whale Shark Experience." Journal of Ecotourism 7, no. 2&3 (December 1, 2008): 208. http://dx.doi.org/10.2167/joe0232.0.

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21

Woo, Mun, Charitha Pattiaratchi, and William Schroeder. "Dynamics of the Ningaloo Current off Point Cloates, Western Australia." Marine and Freshwater Research 57, no. 3 (2006): 291. http://dx.doi.org/10.1071/mf05106.

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The Ningaloo Current (NC) is a wind-driven, northward-flowing current present during the summer months along the continental shelf between the latitudes of 22° and 24°S off the coastline of Western Australia. The southward flowing Leeuwin Current is located further offshore and flows along the continental shelf break and slope, transporting warm, relatively fresh, tropical water poleward. A recurrent feature, frequently observed in satellite images (both thermal and ocean colour), is an anti-clockwise circulation located offshore Point Cloates. Here, the seaward extension of the coastal promon

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22

Kataoka, Takahito, Sébastien Masson, Takeshi Izumo, Tomoki Tozuka, and Toshio Yamagata. "Can Ningaloo Niño/Niña Develop Without El Niño–Southern Oscillation?" Geophysical Research Letters 45, no. 14 (July 16, 2018): 7040–48. http://dx.doi.org/10.1029/2018gl078188.

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23

Mau, Roland. "Managing for Conservation and Recreation: The Ningaloo Whale Shark Experience." Journal of Ecotourism 7, no. 2-3 (October 2008): 213–25. http://dx.doi.org/10.1080/14724040802140550.

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24

Kobryn, Halina T., Kristin Wouters, Lynnath E. Beckley, and Thomas Heege. "Ningaloo Reef: Shallow Marine Habitats Mapped Using a Hyperspectral Sensor." PLoS ONE 8, no. 7 (July 26, 2013): e70105. http://dx.doi.org/10.1371/journal.pone.0070105.

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25

Johnson, Michael S., Jane Prince, Anne Brearley, Natalie L. Rosser, and Robert Black. "Is Tridacna maxima (Bivalvia: Tridacnidae) at Ningaloo Reef, Western Australia?" Molluscan Research 36, no. 4 (May 30, 2016): 264–70. http://dx.doi.org/10.1080/13235818.2016.1181141.

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26

Thébaud, Olivier, L. Richard Little, and Elizabeth Fulton. "Evaluation of management strategies in Ningaloo Marine Park, Western Australia." International Journal of Sustainable Society 6, no. 1/2 (2014): 102. http://dx.doi.org/10.1504/ijssoc.2014.057892.

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27

Taylor, JG. "Seasonal occurrence, distribution and movements of the whale shark, Rhincodon typus, at Ningaloo Reef, Western Australia." Marine and Freshwater Research 47, no. 4 (1996): 637. http://dx.doi.org/10.1071/mf9960637.

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Aerial surveys between 1989 and 1992 demonstrated that large numbers of whale sharks appear on Ningaloo Reef in north-western Australia during autumn, shortly after the coral has undergone mass spawning. This movement into the reef waters would allow whale sharks to capitalize on the increased production of zooplankton brought about as a result of this mass spawning of corals and other marine organisms. Sharks occupied mainly the relatively turbid waters on the reef front, where a northerly current prevailed, rather than the offshore, warmer waters of the southerly flowing Leeuwin Current. The

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28

Sutton, Alicia L., and Lynnath E. Beckley. "Euphausiid assemblages of the oceanographically complex north-west marine bioregion of Australia." Marine and Freshwater Research 68, no. 11 (2017): 1988. http://dx.doi.org/10.1071/mf16334.

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The north-west marine bioregion of Australia, which includes the waters adjacent to the Kimberley and Ningaloo coasts, is influenced by both the Indian and Pacific oceans and has high tropical biodiversity, some of which is conserved in a suite of Marine Protected Areas. In the present study, the epipelagic euphausiid assemblages of this bioregion were investigated and related to the physical and biogeochemical properties of the water column, as well as food availability. Twenty-five euphausiid species were identified, including three new records for Australian waters. Pseudeuphausia latifrons

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29

Onton, K., CA Page, SK Wilson, S. Neale, and S. Armstrong. "Distribution and drivers of coral disease at Ningaloo reef, Indian Ocean." Marine Ecology Progress Series 433 (July 18, 2011): 75–84. http://dx.doi.org/10.3354/meps09156.

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30

Collins, Lindsay B., Zhong Rong Zhu, Karl-Heinz Wyrwoll, and Anton Eisenhauer. "Late Quaternary structure and development of the northern Ningaloo Reef, Australia." Sedimentary Geology 159, no. 1-2 (June 2003): 81–94. http://dx.doi.org/10.1016/s0037-0738(03)00096-4.

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31

Tozuka, Tomoki, Takahito Kataoka, and Toshio Yamagata. "Locally and remotely forced atmospheric circulation anomalies of Ningaloo Niño/Niña." Climate Dynamics 43, no. 7-8 (January 9, 2014): 2197–205. http://dx.doi.org/10.1007/s00382-013-2044-x.

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32

Waite, A. M., V. Rossi, M. Roughan, B. Tilbrook, P. A. Thompson, M. Feng, A. S. J. Wyatt, and E. J. Raes. "Formation and maintenance of high-nitrate, low pH layers in the eastern Indian Ocean and the role of nitrogen fixation." Biogeosciences 10, no. 8 (August 28, 2013): 5691–702. http://dx.doi.org/10.5194/bg-10-5691-2013.

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Abstract. We investigated the biogeochemistry of low dissolved oxygen high-nitrate (LDOHN) layers forming against the backdrop of several interleaving regional water masses in the eastern Indian Ocean, off northwest Australia adjacent to Ningaloo Reef. These water masses, including the forming Leeuwin Current, have been shown directly to impact the ecological function of Ningaloo Reef and other iconic coastal habitats downstream. Our results indicate that LDOHN layers are formed from multiple subduction events of the Eastern Gyral Current beneath the Leeuwin Current (LC); the LC originates fro

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33

Waite, A. M., V. Rossi, M. Roughan, B. Tilbrook, J. Akl, P. A. Thompson, M. Feng, A. S. J. Wyatt, and E. J. Raes. "Formation and maintenance of high-nitrate, low pH layers in the Eastern Indian Ocean and the role of nitrogen fixation." Biogeosciences Discussions 10, no. 3 (March 1, 2013): 3951–76. http://dx.doi.org/10.5194/bgd-10-3951-2013.

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Abstract. We investigate the biogeochemistry of Low Dissolved Oxygen High Nitrate layers forming against the backdrop of several interleaving regional water masses in the Eastern Indian Ocean, off northwest Australia adjacent to Ningaloo Reef. These water masses, including the forming Leeuwin Current, have been shown directly to impact the ecological function of Ningaloo Reef and other iconic coastal habitats downstream. Our results indicate that LODHN layers are formed from multiple subduction events of the Eastern Gyral Current beneath the Leeuwin Current (LC); the LC originates from both th

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34

BRAY, RODNEY A., and THOMAS H. CRIBB. "Stephanostomum tantabiddii n. sp. (Digenea: Acanthocolpidae) from Carangoides fulvoguttatus (Forsskal, 1775) (Perciformes: Carangidae) from Ningaloo Reef, Western Australia." Zootaxa 457, no. 1 (March 9, 2004): 1. http://dx.doi.org/10.11646/zootaxa.457.1.1.

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A new species, Stephanostomum tantabiddii n. sp., is described from the yellowspotted trevally Carangoides fulvoguttatus from Ningaloo Reef, Western Australia. It has 38 45 circum-oral spines and the vitellarium reaches to no less than 17% of the hindbody length from the ventral sucker. It differs from other species of Stephanostomum with these characteristics by various combinations of the ventral hiatus of the circum-oral spine rows, the relatively long pars prostatica and short ejaculatory duct, the elongate body and the wide gaps between the gonads.

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35

Haslam, Veera M., and Mike van Keulen. "Preliminary observations of corallivorous Drupella cornus feeding aggregations at Rottnest Island, Western Australia." Pacific Conservation Biology 26, no. 1 (2020): 98. http://dx.doi.org/10.1071/pc18086.

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Predation by the corallivorous gastropod Drupella cornus is well studied in the tropical and subtropical waters of the Indo-Pacific, including Ningaloo Reef and the Houtman Abrolhos Islands, Western Australia. In 1983, Drupella was not found in the Pocillopora colonies of Rottnest Island (Black and Prince 1983), and there has only been one record of D. cornus on Rottnest Island until today. We show the first feeding aggregations of D. cornus on these higher-latitude reefs of Rottnest Island, and highlight the importance of these findings.

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36

HUNTER, J. A., E. INGRAM, R. D. ADLARD, R. A. BRAY, and T. H. CRIBB. "A cryptic complex of Transversotrema species (Digenea: Transversotrematidae) on labroid, haemulid and lethrinid fishes in the Indo–West Pacific Region, including the description of three new species." Zootaxa 2652, no. 1 (October 21, 2010): 17. http://dx.doi.org/10.11646/zootaxa.2652.1.2.

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Sequences of ITS2 rDNA of 36 individuals of 16 host/parasite/location combinations of transversotrematids from labrid, scarid, haemulid and lethrinid fishes from Heron and Lizard Islands on the Great Barrier Reef and Ningaloo Reef Western off Australia comprised four distinct genotypes. One genotype was associated with three species of Labridae at Heron Island, the second with eight species of Scaridae at Heron Island, the third with two species of Scaridae from Ningaloo, and the fourth with two species of Lethrinidae and one of Haemulidae from Lizard Island. All four forms are broadly morphol

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37

Venables, Stephanie, Frazer McGregor, Lesley Brain, and Mike van Keulen. "Manta ray tourism management, precautionary strategies for a growing industry: a case study from the Ningaloo Marine Park, Western Australia." Pacific Conservation Biology 22, no. 4 (2016): 295. http://dx.doi.org/10.1071/pc16003.

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Localised population declines and increased pressure from fisheries have prompted the promotion of manta ray interaction tourism as a non-consumptive, yet economically attractive, alternative to the unsustainable harvesting of these animals. Unfortunately, however, wildlife tourism activities have the potential to adversely impact focal species. In order to be sustainable, operations must be managed to mitigate negative impacts. A preliminary assessment of reef manta ray, Manta alfredi, behaviour identified short-term behavioural responses during a third of tourism interactions in the Ningaloo

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38

Thums, Michele, Luciana C. Ferreira, Curt Jenner, Micheline Jenner, Danielle Harris, Andrew Davenport, Virginia Andrews-Goff, et al. "Understanding pygmy blue whale movement and distribution off north Western Australia." APPEA Journal 61, no. 2 (2021): 505. http://dx.doi.org/10.1071/aj20202.

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The blue whale (Balaenoptera musculus) is a listed endangered species under the Commonwealth Environment Protection and Biodiversity Conservation Act 1999. A distinct population of blue whales, the eastern Indian Ocean pygmy blue (EIOPB) whale, migrates along the Western Australian coast to the Banda Sea in Indonesia. Their distribution and the delineation of biologically important areas (BIAs) in the north west marine region of the Australian coast are based on limited data with two possible foraging areas identified in the Blue Whale Conservation Management Plan – off Ningaloo and Scott Reef

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39

Curtis, Michael, Simon Holford, Mark Bunch, and Nick Schofield. "Controls on the preservation of Jurassic volcanism in the Northern Carnarvon Basin." APPEA Journal 61, no. 2 (2021): 600. http://dx.doi.org/10.1071/aj20137.

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The Northern Carnarvon Basin (NCB) forms part of the North West Australian margin. This ‘volcanic’ rifted margin formed as Greater India rifted from the Australian continent through the Jurassic, culminating in breakup in the Early Cretaceous. Late Jurassic to Early Cretaceous syn-rift intrusive magmatism spans 45000km2 of the western Exmouth Plateau and the Exmouth Sub-basin; however, there is little evidence of associated contemporaneous volcanic activity, with isolated late Jurassic volcanic centres present in the central Exmouth Sub-basin. The scarcity of observed volcanic centres is not t

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40

PINDER, ADRIAN M., S. M. EBERHARD, and WILLIAM F. HUMPHREYS. "New phallodrilines (Annelida: Clitellata: Tubificidae) from Western Australian groundwater." Zootaxa 1304, no. 1 (August 28, 2006): 31. http://dx.doi.org/10.11646/zootaxa.1304.1.3.

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Four species of phallodriline tubificids (Clitellata: Tubificidae) from karst aquifers and caves along the west coast of the state of Western Australia are the first records of this subfamily from nonmarine waters in the southern hemisphere. Aktedrilus parvithecatus (Erséus 1978) and Pectinodrilus ningaloo n. sp. occur in anchialine groundwater of Cape Range, along with other taxa of marine affinity. Aktedrilus leeuwinensis n. sp. and Aktedrilus podeilema n. sp. occur in caves of the Leeuwin-Naturaliste Ridge and Perth Basin respectively and are the first taxa of marine lineage to have been co

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41

Metaxas, Anna, and Robert E. Scheibling. "Rapid egg transport following coral mass spawning at Ningaloo Reef, Western Australia." Bulletin of Marine Science 92, no. 4 (October 1, 2016): 529–44. http://dx.doi.org/10.5343/bms.2016.1019.

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42

Lozano-Montes, Hector M., John K. Keesing, Monique G. Grol, Michael D. E. Haywood, Mathew A. Vanderklift, Russ C. Babcock, and Kevin Bancroft. "Limited effects of an extreme flood event on corals at Ningaloo Reef." Estuarine, Coastal and Shelf Science 191 (May 2017): 234–38. http://dx.doi.org/10.1016/j.ecss.2017.04.007.

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43

Wood, David, and Michael Hughes. "Tourism accommodation and economic contribution on the Ningaloo Coast of Western Australia." Tourism and Hospitality Planning & Development 3, no. 2 (August 2006): 77–88. http://dx.doi.org/10.1080/14790530600938212.

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44

Tozuka, Tomoki, and Pascal Oettli. "Asymmetric Cloud-Shortwave Radiation-Sea Surface Temperature Feedback of Ningaloo Niño/Niña." Geophysical Research Letters 45, no. 18 (September 27, 2018): 9870–79. http://dx.doi.org/10.1029/2018gl079869.

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45

Bessey, C., and A. K. Cresswell. "Masses of the marine insect Pontomyia oceana at Ningaloo Reef, Western Australia." Coral Reefs 35, no. 4 (August 10, 2016): 1225. http://dx.doi.org/10.1007/s00338-016-1488-y.

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Schönberg, Christine Hanna Lydia, and Jane Fromont. "Sponge gardens of Ningaloo Reef (Carnarvon Shelf, Western Australia) are biodiversity hotspots." Hydrobiologia 687, no. 1 (September 8, 2011): 143–61. http://dx.doi.org/10.1007/s10750-011-0863-5.

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Wilson, S. G., J. J. Polovina, B. S. Stewart, and M. G. Meekan. "Movements of whale sharks (Rhincodon typus) tagged at Ningaloo Reef, Western Australia." Marine Biology 148, no. 5 (November 9, 2005): 1157–66. http://dx.doi.org/10.1007/s00227-005-0153-8.

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Bray, Rodney A., and Thomas H. Cribb. "Ningalooia psammopercae n. g., n. sp. (Digenea: Acanthocolpidae) from the Waigieu seaperch Psammoperca waigiensis (Cuvier) (Perciformes: Latidae) on the Ningaloo Reef, Western Australia." Systematic Parasitology 66, no. 2 (September 13, 2006): 131–35. http://dx.doi.org/10.1007/s11230-006-9056-4.

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Sequeira, Ana M. M., Michele Thums, Kim Brooks, and Mark G. Meekan. "Error and bias in size estimates of whale sharks: implications for understanding demography." Royal Society Open Science 3, no. 3 (March 2016): 150668. http://dx.doi.org/10.1098/rsos.150668.

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Body size and age at maturity are indicative of the vulnerability of a species to extinction. However, they are both difficult to estimate for large animals that cannot be restrained for measurement. For very large species such as whale sharks, body size is commonly estimated visually, potentially resulting in the addition of errors and bias. Here, we investigate the errors and bias associated with total lengths of whale sharks estimated visually by comparing them with measurements collected using a stereo-video camera system at Ningaloo Reef, Western Australia. Using linear mixed-effects mode

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Lester, Emily, Conrad Speed, Dani Rob, Peter Barnes, Kelly Waples, and Holly Raudino. "Using an Electronic Monitoring System and Photo Identification to Understand Effects of Tourism Encounters on Whale Sharks in Ningaloo Marine Park." Tourism in Marine Environments 14, no. 3 (October 23, 2019): 121–31. http://dx.doi.org/10.3727/154427319x15634581669992.

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In-water shark-based tourism is growing worldwide and whale sharks (Rhincodon typus) are one of the most popular targets of this industry. It is important to monitor tourism industries to minimize any potential impacts on target species. At Ningaloo, Western Australia, Electronic Monitoring Systems (EMS) have been installed on licensed tour vessels to collect information on encounters between snorkelers and whale sharks. This study combined data from the EMS with whale shark identification photographs, to assess the impact of in-water tourism on the encounter duration for individual sharks. Du

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