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The Upper Paleolithic (or Upper Palaeolithic) is the third and last subdivision of the Paleolithic or Old Stone Age. Very broadly, it dates to between 50,000 and 12,000 years ago (the beginning of the Holocene ), according to some theories coinciding with the appearance of behavioral modernity in early modern humans , [1] until the advent of ...
Jan 25, 2013 · Discovery’s Monster Squid: The Giant Is Real, due to air this Sunday, might offer a few clues through the first video footage of Architeuthis dux in its deep sea haunts, but marine biologists ...
- Riley Black
The giant squid (Architeuthis dux) is a species of deep-ocean dwelling squid in the family Architeuthidae.It can grow to a tremendous size, offering an example of abyssal gigantism: recent estimates put the maximum size at around 12–13 m (39–43 ft) for females and 10 m (33 ft) for males, from the posterior fins to the tip of the two long tentacles (longer than the colossal squid at an ...
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33 feet. Weight: 440 pounds. Size relative to a bus: IUCN Red List Status: ? Least concern. LC. NT. VU. EN. CR. EW. EX. Least Concern Extinct. Current Population Trend: Unknown. The giant squid...
The Paleolithic or Palaeolithic (/ ˌ p eɪ l i oʊ ˈ l ɪ θ ɪ k, ˌ p æ l i-/ PAY-lee-oh-LITH-ik, PAL-ee-), also called the Old Stone Age (from Ancient Greek παλαιός (palaiós) 'old', and λίθος (líthos) 'stone'), is a period in human prehistory that is distinguished by the original development of stone tools, and which represents almost the entire period of human prehistoric ...
Like octopus and cuttlefish, squid are a type of cephalopod, Greek for “head foot.”. Behind the animal’s head is a soft, elongated mantle: a muscular space containing its organs. Unlike an ...
1. Conservation Status: Least concern. The giant squid is widespread across all oceans, particularly in the North and South Atlantic, and southwestern Pacific ocean. Like all squid, a giant squid has a mantle (torso), eight arms, and two longer tentacles. The giant squid is one of the largest invertebrates on earth.
