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in Earth's recent history there's a fascinating story about enormous creatures that once roamed our planet
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these massive animals called megap ruled the ancient world but their story is one
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of both wonder and tragedy their reign came to a sudden and
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puzzling end welcome to anth media in this video we will understand
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megap Extinction and the thesis that ancient humans played a significant role
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in it about 35,000 years ago the world
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experienced a series of abrupt changes the climate was becoming warmer
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ice sheets melted and sea level was rising at the same time modern humans
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were reaching new environments and using Advanced tools for survival
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humans and megaphonic coexisted for thousands of years hunting these massive
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creatures was a matter of survival cave paintings and ancient artifacts reveal our complex relationship with these
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animals megap the Giants of the prehistoric world existed on Earth for
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millions of years these include huge Marine creatures massive land dinosaurs
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and today's blue whales they they have played crucial roles in shaping ecosystems as Engineers
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Predators herbivores competitors and mutualistic partners megap has faced Extinction in
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the past due to various factors like climate change volcanic eruptions
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asteroid impacts and changes in the atmosphere however in more recent times
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particularly during the late plene and early holos scene the extinction of many
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megap species has been linked to the direct or indirect influence of modern
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humans the early human expansion across the world often coincides with the
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disappearance of these large animals by the time human colonization reached even
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remote Islands numerous species of mammals birds and tortoises had gone
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extinct the loss of megap had significant consequences for ecosystems
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these large animals interacted with many other species including plants parasites
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predators and prey their absence created a Cascade effect impacting the Web of
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Life in various ways the extinction of megap not only
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led to the loss of those animals but also affected species that relied on them this phenomenon is called
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coextinction it particularly affected organisms with close specialized relationships with megap such as
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parasites and mutualistic part Partners Recent research looked at the
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extinction of large mammal species that weighed at least 10 kg over a period from 132,000 to 1,000 years ago they
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found evidence of 177 such species that went extinct globally or on continents
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during this time Africa had 18 extinctions Asia 38
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Australia 26 Europe 19 North America 43 and South America
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62 the study also identified regions where these extinctions were most common
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Texas had the highest number of extinctions about 33 species and Uruguay
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had the highest proportion of Extinction about 78% certain areas like Southern South
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America Southeast North America Western Europe and Southern Australia were identified as Extinction hotspots while
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subsaharan Africa and Southern Asia that had fewer extinctions are considered cold
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spots the late quary period which began around 129,000 years ago and extends to
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the present saw a significant Extinction of megap across much of the
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world earlier in the PTO scene at the beginning of the quader period from
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about 2.6 million years ago both small and large species went extinct and many
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were replaced by new or immigrating species however during the late quary
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most extinctions affected large mammals along with some big birds and reptiles
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while marine animals were mostly unaffected in the 19th century
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scientists like Alfred Russell Wallace and Charles Darwin recognized this large scale
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Extinction Wallace famously noted that we now live in a zoologically impoverished world as many of Earth's
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largest and Most Fascinating creatures have disappeared today there's renewed
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interest in this topic due to concerns about current extinctions and the future of ecosystems some experts argue that we
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are currently witnessing the beginning of a sixth Extinction where many species are at risk of dying
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out scientists have made great progress in studying extinctions by using a
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method called radiocarbon dating this helps them find out how old fossils like
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bones and teeth are knowing the age of these fossils is important for understanding when and where different
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species disappeared other methods like ancient DNA analysis are employed to understand
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the loss of genetic diversity which can cause Extinction however some species like the
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musk ox have survived despite facing similar problems one of the big mysteries in the
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study of megaphon extinctions is why by some regions like North and South America and australasia or hit harder
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than others like subsaharan Africa and Southern Asia where large animals like
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elephants and rhinos still survive though they are now
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endangered understanding the reasons behind these Regional differences is a key challenge for scientists studying
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this period of Extinction factors like climate change habitat loss and human hunting are all believed to have played
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roles in these Extinction let's understand the pattern of Extinction in different regions one by
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one during the last glacial period particularly around the last glacial
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maximum between 21 and 177,000 years a large ice sheet covered much of
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Northwestern Eurasia and extensive glaciers formed in the Alps and other mountain
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ranges the vegetation in regions that are now tundra or Forest was Hur
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dominated step Tundra also known as the mammoth step forests survived only in
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southern areas although the impact of megaphon extinctions in Northern Eurasia has been
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downplayed compared to Regions like North America the losses were still
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significant in areas with good data such as Europe Russia Kazakhstan Mongolia
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northern China and Japan approximately 18 out of 49 large mammal species about
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37% when extinct these included some of the largest animals such as three species of
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elephants and two species of rhinoceroses all of which weighed over 500
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kg the extinction events in Northern Eurasia can be grouped into four phases
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the first wave occurred about 40,000 years ago but these events are less understood due to limited radiocarbon
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data the second wave happened around the start of the last glacial maximum the
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third during the late glacial and early Hol scene and the fourth in the late
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hallene each phase saw The Disappearance of different species over
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time during the early last glacial period several large animals like the
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hippopotamus and straight tusked elephant disappeared from Europe as the climate
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cooled hippos which once ranged as far north as Britain retreated South and
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vanished from the mainland though they survived longer on Mediterranean islands
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and in parts of North Africa the straight tusked elephant was
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common in Europe during a warmer period but may have survived in Iberia until
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about 50,000 years ago with some evidence suggesting it lasted even longer in Northwestern Europe although
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this data needs further confirmation similarly the narrow noed
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rhinoceros once widespread in Europe may have survived until about 45,000 years
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ago in southern regions around the start of the last glacial maximum between 30,000 and
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27,000 years ago several large species went extinct the Cave Bear or ursus Bas
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who was mostly a vegetarian disappeared around 27,500 years
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ago its Extinction is thought to be linked to colder temperatures and the declining quality of
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vegetation in contrast the brown bear survived probably because of its more flexible diet that included both plants
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and meat genetic studies show that cave bears were divided into different species across Europe and Asia with some
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regions overlapping the spotted hyena or Cruda
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Cruda also vanished from northern Eurasia around this time due to colder
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temperatures and fewer prey animals other large animals like the
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cave lion or Panther spala and giant deer or megaloceros gigantus moved
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Eastward as the ice expanded over Europe but survived for a while longer in Japan
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the Nan's elephant or pool oxidon namani went extinct around 28,000 years
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ago there is also some evidence that a sabrtooth cat orium latians survived in
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the North Sea area until about 32,000 years ago though this needs further
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verification the Neanderthals or homon neanderthalensis also disappeared around
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this time the most recent studies suggest they were gone from Europe around 41,000
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to 39,000 years ago although modern humans and Neanderthals coexisted for
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several Millenia allowing some inter breeding neanderthals likely faced
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compet ition from modern humans and worsening climate conditions which contributed to their
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Extinction meanwhile a related group called The dinaso lived in Siberia but
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very little is known about their Extinction timeline from around 4,000 years ago to
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the present several species in northern Eurasia have gone extinct often due to
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changes in climate or human activity for example musox or oios madas
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now found only in Arctic North America and Greenland survived in Northern Siberia until about 3,000 years
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ago the European ass or Equis hydrant Tinus was once widespread across Western
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Eurasia but during the Hol scene its populations became fragmented and
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restricted to southern Europe and Southwest Asia with its last recorded sighting in the caucus about 3,000 years
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ago it's extin Extinction is believed to have been driven by the loss of open habitats due to climate change and over
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hunting by humans the hydron tee ass is depicted in
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Paleolithic cave paintings and Engravings from lasca cave in France as
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well as on Neolithic pottery from Anatolia remains found with cut marks in
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archaeological SES spanning from the Paleolithic to the youngest known remains of the species in the Iron Age
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of Ross the species range including Crimea Italy the Iberian Peninsula and
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Anatolia indicated that it was hunted by people including both modern humans and
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Neanderthals in more recent history species like the arox the wild ancestor
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of domestic cattle went extinct in 1,627 in Poland due to
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hunting lions or Panther a Leo were gone from Southeastern Europe around 2,000
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years ago and they disappeared from the Middle East and North Africa in the past 200
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years leopards or Panther aparis were wiped out from Southern and Central Europe during the holos scene but
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continued to survive in Northern Eurasia China and North Korea as well as Africa
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and Southern Asia there are some species like the extinct camel or camelis nooi and the
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spiral horned Antelope or spal Kay denus that have limited data on when they
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disappeared but it's thought they vanished during a late quinary for other species like the giant
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deer or cegas ceros yab which lived in China and Japan the youngest record is
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around 44,600 years ago the extinction patterns in Northern
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Eurasia are staggered over thousands of years unlike in North America where most
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extinctions occurred rapidly during the late glacial period in Eurasia each species had its
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own complex pattern of range contraction and Extinction likely driven by
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environmental changes rather than direct human activity during the last glacial period
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North America had a rich variety of large mammals partly because of an event called the Great American biotic
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interchange around 3 million years ago North and South America were connected by the esus of Panama allowing animals
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from both continents to migrate between them this included South American
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animals like ground sloths and glyptodon moving North and North American animals heading south additionally North America
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had lower Extinction rates earlier in the Pline compared to Eurasia leading to
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a more diverse megap by the lake quary additionally North America had
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lower Extinction rates earlier in the pla scine compared to Eurasia leading to
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a more diverse megap by the lake quiner however during this period around
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69% of large mammals weighing over 45 kg went extinct including all species of
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horses interestingly although horses went extinct in North America they were
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reintroduced by the Spanish in the 16th century and thrived as feral populations
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such as the Mustangs North America's climate and vegetation changes during the last
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glacial period were similar to Northern Eurasia however the ice sheet in North America was much larger covering most of
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the northern half of the continent for many years this ice sheep
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prevented animals and humans from moving between Alaska and the rest of the
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continent but as the ice began to melt towards the end of the last icial period
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a corridor open between the two main ice sheets allowing animals and people to move between Alaska and what is now the
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contiguous United States by analyzing pollen records scientists have found that vegetation
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remained stable during the last glacial maximum between 21,000 and 17,000 years
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ago but changed rapidly in the late glacial between 16,000 and 11,500 years ago an early holos scene
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between 11,5 8,580 years
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ago after that there was little change until about 500 years ago after 12,000
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years ago as the ice retreated tigga forests spread across much of North
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America humans are thought to have first reached the Americas from Siberia Crossing into Alaska around 14,000 years
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ago they may have been unable to move further south until ice Corridor opened
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but some experts believe people could have traveled along the Pacific coast in boats around 15,000 years
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ago there is archaeological evidence of human presence in Alaska around
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13,500 years ago further south humans are known to have been present in the
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contiguous United States during the Clovis culture which is famous for its distinct stone
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tools this culture existed around 13,200 to 12,800 years ago though some
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evidence suggests that humans may have arrived a few thousand years earlier for example at the buttermilk creek site in
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Texas stone tools have been found dating back to 13,200 to
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15,500 years ago beneath Clovis a layers during alas laal period Alaska
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and the Yukon or Eastern beringia were separated from the rest of North America America by ice sheets making them a
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unique area with their own timeline of species extinctions scientists have gathered
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many radiocarbon dates from megap in this region providing clear evidence of
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when certain species disappeared for example horses or Equis species survived
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until about 14,600 years ago woolly mammoths lived until around
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13,000 400 years ago the cave lion survived until about
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13,300 years ago the SAA Antelope was present until about 14,500 years ago
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today SAA Antelope are found only in parts of Northern Eurasia interestingly woolly mammoths
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also survived on islands like St Paul in the Bearing Sea until about 6,500 years
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ago which is similar to how they survived on Rangel Island into the holos
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scene some other species like the short-faced bear and the saber-tooth cat
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disappeared much earlier before the last glacial maximum the short phed bear vanished
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around 40,000 years ago the saber-tooth cat around 24,700 years ago and the wild ass about
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35,700 years ago these extinctions happened long
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before humans arrived in the area suggesting climate and environmental changes were likely the main
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causes in addition fossils of species like the Western camel Jefferson's
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ground sloth the American Mastadon and the giant beaver found in the Yukon
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likely date back to a warmer period called the last interglacial during this time the
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climate was warmer allowing these species to EXT extend their range further north however as the climate
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cooled again they were probably driven out of the region now let's move to Canada south of
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60° latitude contiguous United States and Northern
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Mexico during the late plyto scine around 35 large animal species went
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extinct in North America there is direct evidence of human hunting for some
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species like the Colombian Mammoth and mastadon as their remains were found with Clovis
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spear points species that disappeared before the last glacial maximum 24,000 years
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ago included giant ground sloth and glyptodont others like the American
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cheetah and Sabertooth vanished around 177,000 18,000 years
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ago most extinctions occurred between 11,000 515,000 years ago including the
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American lion short-faced bear mammoth s mastadons horses and more however older
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radiocarbon dates need updating for accuracy the extinct giant tortoise was
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found as far north as Illinois during the warmer last interglacial period but it likely vanished due to colder
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temperatures in the last glacial period other species that went extinct
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in late Pine North America include several types of Kappa baras and a top
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Pier although they lack precise dating evidence additional studies including
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dating of the short-faced Bear show that it coexisted with humans and was one of
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the last megap to die out around 12,700 to 12,800 years
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ago surviving large mammals in North America today include the polar bear
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grizzly bear mountain lion elk Caribou various deer species and the American
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bison while the Bison nearly faced Extinction in the 19th century due to hunting conservation efforts have helped
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their numbers recover none of these surviving species are currently listed as
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endangered now let's understand Extinction process in South
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America in the late PTO scene South America had a diverse range of animals
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including many unique species that evolved when the continent was isolated ated this period saw significant
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megaphon extinctions with estimates suggesting that about 80% of species became
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extinct notably all horse species disappeared today the largest Native
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mammals in South America are beards to pier and the Loland to Pier weighing only about 350 and 250 kg
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respectively unlike North America and Europe South America wasn't extensively covered by glaciers during the PTO scene
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although there were glaciers in the Andes the last glacial period may have led to a shift towards open grasslands
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which favored grazing animals over tropical forests a key question is why South
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America experienced major extinctions while subsaharan Africa did not despite similar climates and vegetation one
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possibility is that most extinct megap were in southern South America which extends further South in
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Africa research is ongoing but currently there isn't enough reliable dating information to create a clear timeline
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of extinctions fortunately many South American extinctions happened within the
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range of radiocarbon dating making future research
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promising most archaeological sites in South America date to about 13,000 years
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ago or more recently with the Monty verie site in Chile being notable for dating to about
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14,800 years ago this site is recognized as one of the earliest known
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archaeological locations in the Americas based on the dates of
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Extinction of various species three groups have been created Extinction before 18,000 years
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ago includes species like Homen or Giant armadillo glyptodon and
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Hamdon Extinction between 18,000 11,000 years ago includes koronus milodon neum
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and toxodon Extinction between 11,5 8,000 years ago includes Smilodon a
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sabrtooth cat megatherium a giant ground sloth and due to curus AG
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glyptodont however more research is needed to determine if this chronological pattern is accurate some
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species might have survived into the holos scene which began around 11,700 years
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ago the australasian Eco region provides an interesting perspective for understanding megaphon
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Extinction during the pl toine era Australia Tasmania and New Guinea were
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part of a larger land mass called sahle which was connected during periods of low sea
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levels while much of the northern continents were covered by Ice Australia
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experienced exped limited glaciation but underwent significant climate changes alternating between dry and wet
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periods for instance in Queensland at a site called Lynch's crater tropical
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rainforests Thrive from about 130,000 to 78,000 years ago but then changed to
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more drought resistant plants like eucalyp and acaas between 46,000 and 11,000 years ago only to see the
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rainforest return during the Hol scene the first humans ancestors of
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modern Australian aboriginals likely arrived via southeast Asia between 62,000 and 43,000 years ago despite
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lower sea levels they would have needed boats to cross the barriers created by
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water Australia's mamalian fauna was dominated by marsupials along with a few
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egg laying mammals like the Platypus and some unique rodents and B
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the dingo a doglike animal was introduced from Southeast Asia around 3,500 years
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ago during the late Pline around 55 mammal species went extinct in Australia
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and New Guinea including about 40 megapol species the extinction event was
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significant with about 91% of Australia's megap
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disappearing one notable aspect of Australia as extinct mammals is that
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they were generally smaller than their counterparts on other continents this might be due to limited food resources
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and the vast Aid interior of the continent the largest known mammal from
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this time was the giant wombat like theodon which could weigh up to 2
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tons other large extinct species included various giant Kangaroos and a
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marsupial lion known as tholo extinctions also affected non-mean
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species for instance the giant flightless goose called gorus newon and
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the giant monitor lizard called veronis priscus or Megalania are believed to
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have disappeared around the same time most experts believe that nearly
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all megap went extinct around 46,000 years ago which is earlier than in other
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parts of the world the reasons for these extinctions are debated with overkilling
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by humans and climate being two main theories in Australia some important
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surviving species that are considered megap include red kangaroo weighing about 85
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kg Western gray kangaroo and Eastern gray kangaroo these are smaller than the red
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kangaroo emu is a flightless bird that averages around 36 kg but can weigh up
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to 50 kg kg Southern caor can weigh as much as 58
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kg especially females a significant reptilian Survivor
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is the saltwater crocodile which weighs between 400 to 1,000 kg this is the
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largest living reptile in the world and is a major predator of large land animals both in water and on
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land unfortunately several smaller marsupial species have recently gone
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extinct one well-known case is the Tasmanian wolf or Tasmanian tiger the
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Tasmanian government even paid Hunters to kill these animals the last wild Tasmanian tiger
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was shot in 1932 and the last one in captivity died in
29:18
1936 South and Southeast Asia is a diverse region which includes the Indian
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subcontinent Southern China Southeast Asia and the islands of Indonesia and
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the Philippines while there are many records of large prehistoric animals from this
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area it's often unclear when many species went extinct due to poor geological
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data some species that likely became extinct during the late PTO scene in southern China include stegodon
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orientalis a large elephant likee creature pale oxidon patticus another
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extinct elephant OTA bonei a a giant
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panda megga Tyrus Augustus a large tapir and Ultima a type of
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hyena some of these species have also been found in Vietnam and Java claims of other megap surviving
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into more recent times have been re-evaluated and only the bubalis mephistophiles is a short horned water
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buffalo is confirmed to have existed during the early to Middle Hol scene in
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various sites in China there is still much debate and uncertainty about the causes of the
30:33
extinctions that occurred during the late quary period the extinction of large animals
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during the late quader period seems to be closely linked to where humans lived and how long they coexisted with these
30:46
animals rather than just climate changes this pattern is particularly noticeable
30:52
when comparing South America to subsaharan Africa in South America there were
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significant extinctions of large animals despite the climate not changing
31:04
drastically this contrast with subsaharan Africa where there were fewer extinctions despite similar climate
31:12
changes in South America some fluctuations in humidity and habitat
31:18
types might have played a role but they don't seem to be more significant than in
31:23
Africa additionally many of the extinct species in South America were adaptable
31:29
and could switch their diets based on the available food in North America even though
31:36
climate and vegetation didn't change dramatically there were significant extinctions especially around 11,500 to
31:44
10,000 years ago which coincided with the arrival of modern
31:49
humans some experts are arguing that climate change alone couldn't have caused the extinction of large animals
31:56
in Australia they say there's no clear explanation of how increasing dryness or aridity could
32:03
have led to the extinction of big animals without affecting smaller ones or making animals adapt to the changing
32:11
conditions they also mentioned that modern large herbivores can survive in dry and changeable climates because they
32:17
have low energy and water needs eat various foods can live in different habitats and can go without food for a
32:25
while in contrast smaller animals might struggle more when resources become
32:31
scarcer due to climate change overall this suggests that human
32:37
activities such as hunting and habitat modification played a crucial role in
32:43
the extinction of these large animals often more so than climate
32:48
changes those who support climate change as a cause of Extinction have to explain
32:54
why available habitats wouldn't have expanded during Ice Age climate
32:59
they point out that as Australia became drier and sea levels dropped more land
33:04
became exposed along the coast forming large Plains these changes should have
33:12
actually benefited large animals not caused their Extinction they also mentioned that there's no strong
33:18
evidence that the habitats necessary for most big animals got
33:23
smaller one Theory suggests that the disruption of habitats by early humans could explain extinctions changes in
33:31
vegetation and shifts in climate in central Australia between 50,000 and 45,000
33:38
years ago there was a sudden and permanent transformation of Landscapes from tree and shrub savanas to the Arid
33:46
scrub we see today they argue that the only other significant environmental change
33:53
comparable to this happened when Europeans brought in grazing animals like cattle and rabbits they also
34:00
mention evidence of burnt emu eggshells suggesting that humans interacted with extinct
34:06
animals in Northern Australia they found that Landscapes managed by indigenous
34:11
people using fire look different which might have made it harder for large animals to find
34:17
food but hallene is a geological Epoch that began around 11,700 years ago and continues to the
34:25
present day its char characterized by relatively stable climate conditions
34:30
compared to earlier periods monsoons are seasonal winds that bring heavy rainfall during certain
34:37
times of the year crucial for agriculture and ecosystems in those
34:43
regions initially scientists thought that the hallene monsoon failure might have been caused by reaching a specific
34:50
limit or threshold related to water conditions however Recent research
34:55
proposes a different explanation researchers suggest that early human
35:01
activities particularly the systematic burning of vegetation may have played a significant role early humans possibly
35:09
through the intentional use of fire could have altered the landscape by changing the types and distribution of
35:15
plants in dry and semiarid areas the extinction of large animals
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wasn't solely due to climate change extinctions around the world coincide with the arrival of humans suggesting a
35:29
human role the debate has shifted from climate versus humans to how humans did it they
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emphasize that studying how climate change soil conditions landscape fires
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and other ecological factors interact with human activities is crucial they
35:46
also mention that hypotheses should be testable and that various scientific
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methods including ecological and evolutionary theories should be used to
35:57
gain gain a better understanding of this prehistoric Extinction event