Paleontologists ' persuasion of the past tense is usually just a series of snapshots , brief moments in time when condition were right at a particular location for animals or plants to fossilize . Now , however , they have notice a single site that records the development of aliveness over an stupefying 120 million years . considerably yet , it spans the Paleozoic , a peculiarly significant but ill preserved earned run average . The only job is this treasure trove lies in one of the most unaccessible localization on Earth .

On the banks of the Peel River , which further north join the Mackenzie Delta into the Arctic Sea , Science Advancesreports the discovery of rocks commemorate life on the sea floor from 490 to 370 million age ago .

" It ’s unheard of to have that much of Earth ’s history in one place , ”   saidDr Erik Sperlingof Stanford University in astatement . " There ’s nowhere else in the humans that I know of where you’re able to study that long a record of Earth story , where there ’s essentially no change in things like water deepness or basin type . "

Even when condition are ab initio suited for fossilisation to occur , geologic processes usually interrupt what is allow for behind , leaving us with only fragmented records .

The Peel River depots start in theUpper Cambrian , a sentence when atomic number 8 was too scarce to set aside much animal life , and terminate in theMiddle Devonian , when Pisces the Fishes had taken over the seas . Aside from some inadequate interruptions , the entireOrdovicianandSilurianeras are let in . Further study should state us a great deal about the species then exist in these sea , which were not on the bound of the Arctic Circle at the meter as they are now . Such an continuous record can also pretend as a standardization creature for other deposits , help to provide a more precise indication of their timing . “ In ordination to make comparisons throughout these Brobdingnagian swath of our chronicle and understand long - term trends , you call for a uninterrupted record , " Sperling tell .

Stirling ’s paper focuses on what the site reveals about the ascension of O . The other Earth had little to no oxygen in its atmosphere or oceans . TheGreat Oxidation Event2.5 - 2.2 billion years ago changed this , but there was still not enough O to hold today ’s fast - propel , alive lifespan . The timing of the second handsome alteration , when O concentration came to approach those today , is also a topic of considerable precariousness . It may have take place as early on as 800 million years ago , or possibly as little as half that fourth dimension ago . Resolving this question will state us a good deal about the capacity of different case of life to hold out in down in the mouth - atomic number 8 environments .

The paper concludes the atmosphere did not approach its current DoS until afterwards than many scientists have previously thought . " The other animals were still populate in a low oxygen universe , " Sperling said .

worthful as it is , this information was not get ahead easily . The location is so unprocurable Sperling and colleagues had to vanish to the site by helicopter and fight their way through thick brush with machetes . Once there , fieldwork was only possible for a short time before winter put in .

This Week in IFLScience