This is a list of Global Boundary Stratotype Sections and Points. Since 1977, Global Boundary Stratotype Sections and Points (abbreviated GSSPs) are internationally agreed upon reference points on stratigraphic sections of rock which define the lower boundaries of stages on the geologic time scale. They are selected by the International Commission on Stratigraphy based on multiple factors, but their accessibility and the degree to which they are representative of the same boundary on sections worldwide are among the most important.
Since GSSPs require well-preserved sections of rock without interruptions in sedimentation, and since most are defined by different stages of animal life, defining them becomes progressively more difficult as one goes further back in time.
This list is divided first into the geologic eras of the Phanerozoic (the Cenozoic, the Mesozoic, and the Paleozoic) and then into the geologic periods of each era. Each period is marked below the era bar on top of its subdivided epochs and stages. Each stage is assigned an age in mya, an acronym for million years ago, which is the age at which it began. Most of these ages are derived from astronomical cycles in sediments, magnetic data, biostratigraphic data, and radiometric dating methods. The GSSP assigned to each stage is that stage's lower boundary and oldest point.
Ages are given in "million year ago" (mya). They are obtained with different radiometric dating methods depending on the type of rock and its age. Ages that have a tilde (~) prefix are approximate ages for GSSPs that have not been defined or not been accurately dated.
The Status column has a "golden spike" for every GSSP which has been formally agreed by the ICS. Those without have only candidate sections which have not yet been formally ratified. The clock stands for times that are currently defined only by an age.
The "Defining markers" column lists the evidence in the rock used to define the boundary. (Ideally, these are applicable in rock sections worldwide.) Most of the boundaries rely on the fossil record (biologic), paleomagnetic data (magnetic), and/or climate data determined by carbon and oxygen isotopes.
Epoch | Stage | Age (mya) | Status | GSSP location | Defining markers | Geographic Coordinates | References |
---|---|---|---|---|---|---|---|
Holocene | |||||||
Meghalayan | 0.0042 | Mawmluh Cave, Meghalaya, India |
| 25°15′44″N91°42′54″E / 25.2622°N 91.7150°E | [1] [2] | ||
Northgrippian | 0.0082 | NGRIP1 ice core, |
| 75°06′00″N42°19′12″W / 75.1000°N 42.3200°W | [1] | ||
Greenlandian | 0.0117 | NGRIP2 ice core, |
| 75°06′00″N42°19′12″W / 75.1000°N 42.3200°W | [1] [3] | ||
Pleistocene | |||||||
Upper/Late | 0.129 | - |
| - | - | ||
Chibanian | 0.774 | Chiba, Japan |
| 35°17′39″N140°08′47″E / 35.2943°N 140.1465°E | [4] | ||
Calabrian | 1.8 | Vrica Section, Calabria, Italy |
| 39°02′19″N17°08′05″E / 39.0385°N 17.1348°E | [5] | ||
Gelasian | 2.58 | Monte San Nicola Section, |
| 37°08′47″N14°12′16″E / 37.146468°N 14.204562°E | [6] |
Epoch | Stage | Age (mya) | Status | GSSP location | Defining markers | Geographic Coordinates | References |
---|---|---|---|---|---|---|---|
Pliocene | |||||||
Piacenzian | 3.6 | Punta Piccola Section, Porto Empedocle, Sicily, Italy |
| 37°17′22″N13°29′29″E / 37.289386°N 13.491443°E | [7] | ||
Zanclean | 5.333 | Heraclea Minoa section Heraclea Minoa, Cattolica Eraclea, Sicily, Italy |
| 37°23′33″N13°16′52″E / 37.392435°N 13.281052°E | [8] | ||
Miocene | |||||||
Messinian | 7.246 | Oued Akrech section, |
| 33°55′30″N6°48′33″W / 33.925050°N 6.809047°W | [9] | ||
Tortonian | 11.63 | Monte dei Corvi Beach section, Ancona, Italy |
| 43°35′14″N13°33′58″E / 43.587242°N 13.566148°E | [10] | ||
Serravallian | 13.82 | Ras il Pellegrin section, |
| 35°54′50″N14°20′10″E / 35.9139°N 14.3361°E | [11] | ||
Langhian | 15.98 | At 17.84 m in the 'Lower La Vedova Beach' section, Ancona, Italy |
| 43°35′31″N13°33′44″E / 43.5919°N 13.5623°E | [4] | ||
Burdigalian | 20.44 | Candidate sections:
|
| - | [4] | ||
Aquitanian | 23.03 | Lemme-Carrosio Section, Carrosio, Italy |
| 44°39′36″N8°50′21″E / 44.6601°N 8.83928°E | [12] |
Epoch | Stage | Age (mya) | Status | GSSP location | Defining markers | Geographic Coordinates | References |
---|---|---|---|---|---|---|---|
Oligocene | |||||||
Chattian | 27.82 | Monte Cagnero, Central Apennines, Italy | Biological: last occurrence of the planktonic foraminifer Chiloguembelina (Base of Foram Zone P21b) | 43°38′48″N12°28′04″E / 43.646748°N 12.467771°E | [13] | ||
Rupelian | 33.9 | Massignano quarry section, Massignano, Ancona, Italy |
| 43°32′10″N13°35′33″E / 43.536038°N 13.592499°E | [14] | ||
Eocene | |||||||
Priabonian | 37.71 | Alano section, Piave river, Venetian Prealps, Belluno, Italy |
| 45°54′51″N11°55′05″E / 45.9141°N 11.9180°E | [15] | ||
Bartonian | 41.2 | Contessa highway section Gubbio, Central Apennines, Italy |
| 43°22′47″N12°33′44″E / 43.37972°N 12.56219°E | - | ||
Lutetian | 47.8 | Gorrondatxe sea-cliff section, Western Pyrenees, Basque Country, Spain |
| 43°22′47″N3°00′51″W / 43.3796°N 3.0143°W | [16] | ||
Ypresian | 56 | Dababiya section, |
| 25°30′00″N32°31′52″E / 25.5000°N 32.5311°E | [17] [18] | ||
Paleocene | |||||||
Thanetian | 59.2 | Zumaia Section, Basque Country, Spain |
| 43°17′59″N2°15′39″W / 43.2996°N 2.2609°W | [19] | ||
Selandian | 61.6 | Zumaia Section, Basque Country, Spain |
| 43°17′57″N2°15′40″W / 43.2992°N 2.2610°W | [19] | ||
Danian | 66 | El Kef Section, |
| 36°09′13″N8°38′55″E / 36.1537°N 8.6486°E | [20] |
Epoch | Stage | Age (mya) | Status | GSSP location | Defining markers | Geographic Coordinates | References |
---|---|---|---|---|---|---|---|
Pennsylvanian | |||||||
Gzhelian | 303.7 | Candidate sections:
|
| - | [4] | ||
Kasimovian | 307 | Candidate sections:
|
| - | [4] | ||
Moscovian | 315.2 | Candidate sections:
|
| - | [4] | ||
Bashkirian | 323.2 | Arrow Canyon, Nevada, United States |
| 36°44′00″N114°46′40″W / 36.7333°N 114.7778°W | [46] | ||
Mississippian | |||||||
Serpukhovian | 330.9 | Candidate sections: |
| - | [4] | ||
Visean | 346.7 | Pengchong Section, Guangxi, China |
| 24°26′00″N109°27′00″E / 24.4333°N 109.4500°E | [4] | ||
Tournaisian | 358.9 | La Serre, Montagne Noire, France |
| 43°33′20″N3°21′31″E / 43.55554°N 3.35868°E | [47] |
Era | Period | Age (mya) | Status | GSSP location | Defining markers | Geographic Coordinates | References |
---|---|---|---|---|---|---|---|
Neoproterozoic | |||||||
Ediacaran | ~635 | Enorama Creek section |
| 31°19′53″S138°38′00″E / 31.3314°S 138.6334°E | [78] | ||
Cryogenian | ~720 | Defined chronometrically with an interim calibrated age of ca. 720 Ma. GSSP is in progress. |
| - | [79] | ||
Tonian | 1000 | Defined chronometrically | - | - | [80] | ||
Mesoproterozoic | |||||||
Stenian | 1200 | Defined chronometrically | - | - | [80] | ||
Ectasian | 1400 | Defined chronometrically | - | - | [80] | ||
Calymmian | 1600 | Defined chronometrically | - | - | [80] | ||
Paleoproterozoic | |||||||
Statherian | 1800 | Defined chronometrically | - | - | [80] | ||
Orosirian | 2050 | Defined chronometrically | - | - | [80] | ||
Rhyacian | 2300 | Defined chronometrically | - | - | [80] | ||
Siderian | 2500 | Defined chronometrically | - | - | [80] |
Eon | Era | Age (mya) | Status | GSSP/GSSA location | Defining markers | Geographic Coordinates | References |
---|---|---|---|---|---|---|---|
Archean | |||||||
Neoarchean | 2800 | - | Defined chronometrically | - | - | ||
Mesoarchean | 3200 | - | Defined chronometrically | - | - | ||
Paleoarchean | 3600 | - | Defined chronometrically | - | - | ||
Eoarchean | 4031 | Along the Acasta River, Northwest Territories, Canada | Defined chronometrically Ten oldest U-Pb zircon ages | 65°10′26″N115°33′14″W / 65.1738°N 115.5538°W | [4] | ||
Hadean | - | 4567.3 | - | Defined chronometrically | - | [4] |
The Zanclean is the lowest stage or earliest age on the geologic time scale of the Pliocene. It spans the time between 5.332 ± 0.005 Ma and 3.6 ± 0.005 Ma. It is preceded by the Messinian Age of the Miocene Epoch, and followed by the Piacenzian Age.
The Tremadocian is the lowest stage of Ordovician. Together with the later Floian Stage it forms the Lower Ordovician Epoch. The Tremadocian lasted from 485.4 to 477.7 million years ago. The base of the Tremadocian is defined as the first appearance of the conodont species Iapetognathus fluctivagus at the Global Boundary Stratotype Section and Point (GSSP) section on Newfoundland.
The Albian is both an age of the geologic timescale and a stage in the stratigraphic column. It is the youngest or uppermost subdivision of the Early/Lower Cretaceous Epoch/Series. Its approximate time range is 113.0 ± 1.0 Ma to 100.5 ± 0.9 Ma. The Albian is preceded by the Aptian and followed by the Cenomanian.
The Furongian is the fourth and final epoch and series of the Cambrian. It lasted from 497 to 485.4 million years ago. It succeeds the Miaolingian series of the Cambrian and precedes the Lower Ordovician Tremadocian Stage. It is subdivided into three stages: the Paibian, Jiangshanian and the unnamed 10th stage of the Cambrian.
The Messinian is in the geologic timescale the last age or uppermost stage of the Miocene. It spans the time between 7.246 ± 0.005 Ma and 5.333 ± 0.005 Ma. It follows the Tortonian and is followed by the Zanclean, the first age of the Pliocene.
Calabrian is a subdivision of the Pleistocene Epoch of the geologic time scale, defined as 1.8 Ma—774,000 years ago ± 5,000 years, a period of ~1.026 million years.
The Serravallian is, in the geologic timescale, an age or a stage in the middle Miocene Epoch/Series, which spans the time between 13.82 Ma and 11.63 Ma. The Serravallian follows the Langhian and is followed by the Tortonian.
The Tortonian is in the geologic time scale an age or stage of the late Miocene that spans the time between 11.608 ± 0.005 Ma and 7.246 ± 0.005 Ma. It follows the Serravallian and is followed by the Messinian.
In the geologic timescale, the Sinemurian is an age and stage in the Early or Lower Jurassic Epoch or Series. It spans the time between 199.5 ±0.3 Ma and 192.9 ±0.3 Ma. The Sinemurian is preceded by the Hettangian and is followed by the Pliensbachian.
The Pliensbachian is an age of the geologic timescale and stage in the stratigraphic column. It is part of the Early or Lower Jurassic Epoch or Series and spans the time between 192.9 ±0.3 Ma and 184.2 ±0.3 Ma. The Pliensbachian is preceded by the Sinemurian and followed by the Toarcian.
The Darriwilian is the upper stage of the Middle Ordovician. It is preceded by the Dapingian and succeeded by the Upper Ordovician Sandbian Stage. The lower boundary of the Darriwilian is defined as the first appearance of the graptolite species Undulograptus austrodentatus around 467.3 million years ago. It lasted for about 8.9 million years until the beginning of the Sandbian around 458.4 million years ago. This stage of the Ordovician was marked by the beginning of the Andean-Saharan glaciation.
The Katian is the second stage of the Upper Ordovician. It is preceded by the Sandbian and succeeded by the Hirnantian Stage. The Katian began 453 million years ago and lasted for about 7.8 million years until the beginning of the Hirnantian 445.2 million years ago. During the Katian the climate cooled which started the Late Ordovician glaciation.
The Sandbian is the first stage of the Upper Ordovician. It follows the Darriwilian and is succeeded by the Katian. Its lower boundary is defined as the first appearance datum of the graptolite species Nemagraptus gracilis around 458.4 million years ago. The Sandbian lasted for about 5.4 million years until the beginning of the Katian around 453 million years ago.
The Dapingian is the third stage of the Ordovician period and the first stage of the Middle Ordovician series. It is preceded by the Floian and succeeded by the Darriwilian. The top of the Floian is defined as the first appearance of the conodont species Baltoniodus triangularis which happened about 470 million years ago. The Dapingian lasted for about 2.7 million years until about 467.3 million years ago.
The Jiangshanian is the middle stage of the Furongian series. It follows the Paibian Stage and is succeeded by the still unnamed Stage 10 of the Cambrian. The base is defined as the first appearance of the trilobite Agnostotes orientalis which is estimated to be 494 million years ago. The Jiangshanian lasted until approximately 489.5 million years ago.
The Guzhangian is an uppermost stage of the Miaolingian Series of the Cambrian. It follows the Drumian Stage and precedes the Paibian Stage of the Furongian Series. The base is defined as the first appearance of the trilobite Lejopyge laevigata around 500.5 million years ago. The Guzhangian-Paibian boundary is marked by the first appearance of the trilobite Glyptagnostus reticulatus around 497 million years ago.
The Drumian is a stage of the Miaolingian Series of the Cambrian. It succeeds the Wuliuan and precedes the Guzhangian. The base is defined as the first appearance of the trilobite Ptychagnostus atavus around 504.5 million years ago. The top is defined as the first appearance of another trilobite Lejopyge laevigata around 500.5 million years ago.
The Wuliuan stage is the fifth stage of the Cambrian, and the first stage of the Miaolingian Series of the Cambrian. It was formally defined by the International Commission on Stratigraphy in 2018. Its base is defined by the first appearance of the trilobite species Oryctocephalus indicus; it ends with the beginning of the Drumian Stage, marked by the first appearance of the trilobite Ptychagnostus atavus around 504.5 million years ago.
Stage 10 of the Cambrian is the still unnamed third and final stage of the Furongian series. It follows the Jiangshanian and precedes the Ordovician Tremadocian Stage. The proposed lower boundary is the first appearance of the trilobite Lotagnostus americanus around 489.5 million years ago, but other fossils are also being discussed. The upper boundary is defined as the appearance of the conodont Iapetognathus fluctivagus which marks the beginning of the Tremadocian and is radiometrically dated as 485.4 million years ago.
The Miaolingian is the third Series of the Cambrian Period, and was formally named in 2018. It lasted from about 509 to 497 million years ago and is divided in ascending order into 3 stages: the Wuliuan, Drumian, and Guzhangian. The Miaolingian is preceded by the unnamed Cambrian Series 2 and succeeded by the Furongian series.
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