Few discussions in geology can occur without reference to geologic time. Geologic time is often dicussed in two forms:
Relative time ("chronostratic") -- subdivisions of the Earth's geology in a specific order based upon relative age relationships (most commonly, vertical/stratigraphic position). These subdivisions are given names, most of which can be recognized globally, usually on the basis of fossils.
Absolute time ("chronometric") -- numerical ages in "millions of years" or some other measurement. These are most commonly obtained via radiometric dating methods performed on appropriate rock types.
Think of relative time as physical subdivisions of the rock found in the Earth's stratigraphy, and absolute time as the measurements taken upon those to determine the actual time which has expired. Absolute time measurements can be used to calibrate the relative time scale, producing an integrated geologic or "geochronologic" time scale.
It is important to realize that with new information about subdivision or correlation of relative time, or new measurements of absolute time, the dates applied to the time scale can and do change. Revisions to the relative time scale have occurred since the late 1700s. The numerically calibrated geologic time scale has been continuously refined since approximately the 1930s (e.g., Holmes, 1937), although the amount of change with each revision has become smaller over the decades (see fig. 1.5 and 1.6 of Harland et al.) and a few numerical estimates were available previously (but often for the duration of the entire scale rather than its individual subdivisions).
In addition, like any good scientific measurement, every dated boundary has an uncertainty associated with it, expressed as "+- X millions of years". These can not be included in the diagram for practical reasons, but can be found in Harland et al., 1990, along with a detailed description of the history of earlier-proposed time scales and the terminology, methodology and data involved in constructing this geological time scale.
Because of continual refinement, none of the values depicted in this diagram should be considered definitive, eventhough some have not changed significantly in a long time and are very well constrained (e.g., the Cretaceous/Tertiary boundary has been at 65+-1 Ma for decades, and has been tested innumerable times, with almost all dates somewhere between 64 and 66 million years). The overall duration and relative length of these large geologic intervals is unlikely to change much, but the precise numbers may "wiggle" a bit as a result of new data.
This gelogical time scale is based upon Harland et al., 1990, but with the Precambrian/Cambrian boundary modified according to the most recently-published radiometric dates on that interval, revising the boundary from 570+-15 million years to 543+-1 million years ago (Grotzinger et al., 1995). Other changes have been proposed since 1990 (e.g., revision of the Cretaceous by Obradovich, 1993), but are not incorporated because they are relatively small.
The time scale is depicted in its traditional form with oldest at the bottom and youngest at the top -- the present day is at the zero mark. Geologic time is finely subdivided through most of the Phanerozoic (see Harland et al., 1990 for details), but most of the finer subdivisions (e.g., epochs) are commonly referred to by non-specialists only in the Tertiary. Because of the vast difference in scale, the younger intervals have been successively expanded to the right to show some of these finer subdivisions.
geological time scale
Blatt, H.; Berry, W.B.N.; and Brande, S., 1991. Principles of Stratigraphic Analysis. Blackwell Scientific Publications: Boston, p.1-512. ISBN 0-86542-069-6 [Chapter 4 provides an introduction to geologic time. This is a good starting point to get the basic principles.]
Grotzinger, J.P.; Bowring, S.A.; Saylor, B.Z.; and Kaufman, A.J., 1995 (Oct.27). Biostratigraphic and geochronologic constraints on early animal evolution. Science, v.270, p.598-604. [The most recent revision of the age of the Precambrian/Cambrian boundary.]
Harland, W.B.; Armstrong, R.L.; Cox, A.V.; Craig, L.E.; Smith, A.G.; and Smith, D.G., 1990. A geologic time scale, 1989 edition. Cambridge University Press: Cambridge, p.1-263. ISBN 0-521-38765-5 [One of the more recent compilations of the entire geologic time scale.]
Holmes, A., 1937. The Age of the Earth (new edition, revised). Nelson:London, p.1-263. [One of the earlier attempts at an integrated geochronologic time scale.]
Obradovich, J.D., 1993. A Cretaceous time scale. IN: Caldwell, W.G.E. and Kauffman, E.G. (eds.), Evolution of the Western Interior Basin. Geological Association of Canada, Special Paper 39, p.379-396. [Proposes revisions to the Cretaceous time scale at the resolution of stages (finer divisions than shown on diagram above) and sub-stages.]
Автор(ы): Harris Nic Издательство: Cambridge, 2014 г.
Цена: 697 руб. Купить
Determining the greatest invention of all time invites the greatest debate. From the internet to antibiotics, this reader explores our most significant contributions to education, technology, medicine, and transportation.
Автор(ы): Gaiman Neil Издательство: Bloomsbury, 2014 г.
Цена: 850 руб. Купить
You know what it's like when your mum goes away on a business trip and Dad's in charge. She leaves a really, really long list of what he's got to do. And the most important thing is DON'T FORGET TO GET THE MILK. Unfortunately, Dad forgets. So the next morning, before breakfast, he has to go to the corner shop, and this is the story of why it takes him a very, very long time to get back. Featuring: Professor Steg (a time-travelling dinosaur), some green globby things, the Queen of the Pirates, the famed jewel that is the Eye of Splod, some wumpires, and a perfectly normal but very important carton of milk. The award-laden, bestselling Neil Gaiman, author of The Ocean at the End of the Lane, Stardust, Neverwhere, The Graveyard Book and Coraline, brings his biggest ever publishing year to a spectacular conclusion with this gloriously entertaining novel about time-travel, dinosaurs, milk and dads.
Автор(ы): Crow Nosy Издательство: Little, Brown and Company, 2011 г.
Цена: 1321 руб. Купить
Pip and Posy are typical toddlers: they are best friends and they have fun... but sometimes, just like any other toddler, they get cross and sad, so sometimes it takes friendship, sharing and understanding - and a cuddle - to make things better. In Pip and Posy and the Little Puddle Pip comes to play at Posy's house. They have such a lovely time after their mid-afternoon snack and drink that Pip forgets he needs to go to the loo, and soon there's a little puddle on the floor. But everyone has accidents sometimes, so Posy mops it up, and lends him some clothes. The next time Pip needs a wee, he does it in the potty all by himself.
Цена: 447 руб. Купить
This cute Little Library includes six mini Peppa Pig classic fairy tale adventure books in a beautiful slipcase box. Join Princess Peppa Pig and Prince George in their wonderful fairy tale castle up in the clouds and read their stories time and time again. Six books make a jigsaw. Books: The Royal Party Sleepy Princess The King, the Cook and the Wizard George's Dragon Sir George the Brave Princess Peppa