― David Attenborough, Oceans
Diplomoceras (Double Horn) is a genus of diplomoceratid ammonite cephalopod that lived in various parts of the world (but is primarily known from the López de Bertodano Formation of Seymour Island, Antarctica), 83.6 - 66 million years ago, from the Campanian to the Maastrichtian stage of the Late Cretaceous Period. It is distinct among ammonites for its paperclip-shaped shell. The species featured on Prehistoric Planet isn't specified, though given its size, it is likely Diplomoceras maximum, the largest known species.
Paleobiology[]
Size and Physique[]
Diplomoceras is a large ammonite with a shell around 1.5 - 1.8 meters (5 - 6 feet) long,[2][4] recognizable for its resemblance to a paperclip. If it were to be straightened, the shell would measure 3 - 4 meters (10 - 13 feet) long,[2] and the body chamber (the part that actually contains the animal) would be 2 meters (6 feet, 7 inches) long.[5]
Growth and Lifespan[]
Diplomoceras was originally believed to live for up to ten years based on its sinusoids (curves), each of which indicates 1.5 years of quick shell growth,[2] a lifespan matching the brief ones of other cephalopods like modern-day species of octopus, which live for under five years. Prehistoric Planet itself depicts this in the fifth segment of Coasts, with the short lives of scaphitids coming to an end soon after mating and reproduction. However, a more recent study in 2020, based on the ribs of the animal's shell (with each rib representing a year of growth), suggests that Diplomoceras may have grown slowly over the course of approximately 200 years.[6]
Paleoecology[]
Paleoenvironment[]
Main: López de Bertodano Formation, Tethys Ocean
Main: López de Bertodano Formation, Tethys Ocean

― David Attenborough, Oceans
Diplomoceras maximum lived 66 million years ago in the López de Bertodano Formation of Seymour Island, which showed that the waters surrounding Antarctica were warmer than they are in the modern day, though, at 4 - 12 degrees Celsius (39.2 - 54 degrees Fahrenheit), the area was still very much cold, hence, the seas of Antarctica would have still been plausibly covered in sheets of ice, just as depicted in the sixth segment of Oceans.[7] Prehistoric Planet instead depicts Diplomoceras maximum in the Tethys Ocean of Europe. This is not entirely implausible given the wide range of habitats that ammonites can live in, and Diplomoceras specimens have also been found in other places like Japan.[1][3]
Diplomoceras was rendered extinct by the Cretaceous-Paleogene Extinction Event 66.043 million years ago,[8] a catastrophe that wiped out three-quarters of all life on Earth, including all non-avian dinosaurs, pterosaurs, plesiosaurs, and mosasaurs. However, while many ammonites like Diplomoceras perished by the end of the Cretaceous, a few of them, like certain species of Baculites[9] and Pachydiscus survived into the Danian stage of the Early Paleocene Period, approximately 61.6 million years ago.
Feeding Preferences[]
Not much is known about the behavior and preferences of Diplomoceras. However, cold methane vents closely associated with the fossil, coupled with the cephalopod's vertically-oriented shell, indicate that Diplomoceras lived close to the bottom of the ocean, and was thus likely a benthivore, a bottom-feeding animal that filtered food on or near the sea floor.[2][4] One of the tiny creatures that Diplomoceras may have plucked from the bottom of the ocean is Rotularia, a serpulid polychaete worm approximately 13 centimeters (5 inches) in length.
Appearances[]
Oceans[]
TBA
Uncovered: What Do We Really Know About Ammonites?[]
TBA
References[]
General[]
- ↑ 1.0 1.1 The Last Surviving Ammonoid at the end of the Cretaceous in the North Pacific Region
- ↑ 2.0 2.1 2.2 2.3 2.4 2.5 2.6 2.7 Discovery of a remarkably complete specimen of the giant cephalopod Diplomoceras maximum from the Late Cretaceous of Seymour Island, Antarctica
- ↑ 3.0 3.1 Late Campanian–early Maastrichtian heteromorph-dominated ammonoid assemblages of the Nakaminato Group, central Honshu, Japan: biostratigraphic and paleontological implications
- ↑ 4.0 4.1 4.2 4.3 Giant Heteromorph Ammonite
- ↑ 5.0 5.1 Discovery of a remarkably complete specimen of the giant cephalopod Diplomoceras maximum from the Late Cretaceous of Seymour Island, Antarctica
- ↑ 6.0 6.1 Large squid-like creature that looked like a giant paperclip lived for 200 years — 68 million years ago
- ↑ Late Cretaceous winter sea ice in Antarctica?
- ↑ Dinosaur extinction battle flares
- ↑ Ammonites on the Brink of Extinction: Diversity, Abundance, and Ecology of the Order Ammonoidea at the Cretaceous/Paleogene (K/Pg) Boundary
Prehistoric Planet[]
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Marine Reptiles and Birds | |
Mosasaurs | |
Plesiosaurs | |
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Other Marine Life | |
Ammonites |
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Africa | |
Madagascar | |
Morocco | |
America, North | |
Alberta, Canada |
Horseshoe Canyon Formation |
Scollard Formation | |
United States |
Hell Creek and Lance Formations |
Javelina Formation | |
Prince Creek Formation | |
Western Interior Seaway |
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America, South | |
Argentina | |
Brazil | |
Others | |
Antarctica | |
López de Bertodano Formation |
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Snow Hill Island Formation |
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Asia | |
China | Nanxiong Formation |
Songliao Basin | |
India | |
Japan | |
Mongolia | Barun Goyot Formation |
Nemegt Formation | |
Russia | |
Europe | |
Hațeg Island |
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Tethys Ocean |
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Others | |
Oceania | |
New Zealand |
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