Mugiliformes - Mullets
Perciformes - Perches
Carangiformes - Jacks
Istiophoriformes - Barracudas
Scorpaeniformes - Mail-cheeked fishes
Lamniformes - Mackerel sharks
Carcharhiniformes - Ground sharks
Orectolobiformes - Carpet shark
Myliobatiformes - Stingrays
Scombriformes - Mackerels
Anguilliformes - Eels and morays
Tetraodontiformes - Puffers and filefishes
Holocentriformes - Squirrelfishes
Lophiiformes - Anglerfishes
Acanthuriformes - Surgeonfishes
Labriformes - Wrasses
Gobiiformes - Gobies
Lampriformes - Lamprids
Mulliformes - Goatfishes
Gadiformes - Cods
Centrarchiformes - Basses and sunfishes
Callionymiformes - Dragonets
Syngnathiformes - Pipefishes and Seahorses
Spariformes - Breams and porgies
Echinorhiniformes - Bramble sharks
Saccopharyngiformes - Swallowers and Gulpers
Gonorynchiformes - Milkfishes
Beryciformes - Sawbellies
Ophidiiformes - Cusk-eels
Kurtiformes - Nurseryfishes & Cardinalfishes
Acropomatiformes - Oceanic basses
Beloniformes - Needlefishes
Trachiniformes - Weeverfishes
Pleuronectiformes - Flatfishes
Aulopiformes - Grinners
Blenniiformes - Blennies
The Celebes Sea, or Sulawesi Sea, of the western Pacific Ocean is bordered on the north by the Sulu Archipelago and Sulu Sea and Mindanao Island of the Philippines, on the east by the Sangihe Islands chain, on the south by Sulawesis Minahasa Peninsula, and on the west by northern Kalimantan in Indonesia.
It extends 420 miles (675 km) north-south by 520 mi (840 km) east-west and has a total surface area of 110,000 square miles (280,000 km2), to a maximum depth of 20,300 feet (6,200 m).
South of the Cape Mangkalihat, the sea opens southwest through the Makassar Strait into the Java Sea.
The Celebes Sea is a piece of an ancient ocean basin that formed 42 million years ago in a locale removed from any landmass. By 20 million years ago, earth crust movement had moved the basin close enough to the Indonesian and Philippine volcanoes to receive emitted debris. By 10 million years ago the Celebes Sea was inundated with continental debris, including coal, which was shed from a growing young mountain on Borneo and the basin had docked against Eurasia.
The border between the Celebes and the Sulu Sea is at the Sibutu-Basilan Ridge. Strong ocean currents, deep sea trenches and seamounts, combined with active volcanic islands, result in complex oceanographic features.
