Resolution Guyot
21°15′0″N 174°20′0″E / 21.25000°N 174.33333°E
Resolution Guyot (formerly known as Huevo) is a guyot (tablemount) in the underwater Mid-Pacific Mountains in the Pacific Ocean. It is a circular flat mountain, rising 500 metres (1,600 ft) above the seafloor to a depth of about 1,320 metres (4,330 ft), with a 35-kilometre-wide (22 mi) summit platform. The Mid-Pacific Mountains lie west of Hawaii and northeast of the Marshall Islands, but at the time of its formation, the guyot was located in the Southern Hemisphere.
The guyot was probably formed by a hotspot in today's French Polynesia before plate tectonics shifted it to its present-day location. The Easter, Marquesas, Pitcairn and Society hotspots, among others, may have been involved in the formation of Resolution Guyot. Volcanic activity has been dated to have occurred 107–129 million years ago and formed a volcanic island that was subsequently flattened by erosion. Carbonate deposition commenced, forming an atoll-like structure and a carbonate platform.
The platform emerged above sea level at some time between the
Name and research history
Resolution Guyot was informally known as Huevo Guyot
Geography and geology
Local setting
Resolution Guyot is one of the western Mid-Pacific Mountains, located west of Hawaii, north-northeast of the Marshall Islands.[7] Unlike conventional Pacific Ocean island chains,[8] the Mid-Pacific Mountains are a group of oceanic plateaus with guyots[9] (also known as tablemounts)[10]) that become progressively younger towards the east.[11] Other guyots in the Mid-Pacific Mountains are Sio South, Darwin, Thomas, Heezen, Allen, Caprina, Jacqueline and Allison.[12]
The seamount is about 500 metres (1,600 ft) high and rises from a raised seafloor
The guyot rises from a seafloor of Jurassic age[11] (201.3 ± 0.2 – ca. 145 million years ago[21]) that might be as much as 154 million years old.[9] Terrestrial organic material on the seafloor around Resolution Guyot originated from when it was still an island,[22] and carbonate sediments swept away from the guyot collected on the surrounding seafloor.[23][24]
Regional setting
The
The formation of many seamounts has been explained by the
Composition
Rocks found at Resolution Guyot include
The carbonates occur in the form of
Organic materials[e] found in rock samples from Resolution Guyot[56] appear to be mainly of marine origin.[58] Some of the organic matter comes from microbial mats and vegetated islands,[59] including wood[60] and plant remains.[14]
Clays found on Resolution Guyot are characterized as
Geologic history
Cretaceous graphical timeline | ||||
−140 — – −130 — – −120 — – −110 — – −100 — – −90 — – −80 — – −70 — – |
| |||
Although
Volcanic phase
Eruptions in the area built a pile of volcanic rocks, including stacks of
Platform carbonates and reefs
Between the Hauterivian (ca. 132.9 – ca. 129.4 million years ago[21]) and Albian (ca. 113 – 100.5 million years ago[21]), about 1,619 metres (5,312 ft) of carbonate was deposited on the volcanic structure,[47] eventually completely burying it during the Albian.[74] About 14 individual sequences of carbonates have been identified in drill cores.[75] The carbonate sedimentation probably began in the form of shoals surrounding a volcanic island[76] and lasted for about 35 million years,[77] accompanied by perhaps 0.046 millimetres per year (0.0018 in/year) of subsidence.[78] It is likely that the present-day carbonate platform contains only a fraction of the originally deposited carbonate, most of the carbonate having disappeared.[79] During this time, Resolution Guyot underwent little latitudinal plate motion; from the magnetization it appears that it was stably located at about 13° southern latitude between the Hauterivian and Aptian.[80]
Its carbonate platform cannot be reconstructed as only small parts have been studied, but some conclusions can be made.
The Cretaceous Apulian Carbonate Platform in Italy and the Urgonian Formation in France have been compared to the Resolution Guyot carbonates. All these platforms were located in Tethyan seas[87] and several formations in these three carbonate environments are correlated;[88] for example, the fauna identified on Resolution Guyot resembles that from other Northern Hemisphere platforms.[89] Analogies also exist to platforms in Venezuela.[88]
-
A beach and shallow water, Cook Islands
-
Spaceborne image of mudflats and tidal channels on present-day Long Island, Bahamas; the former morphology of Resolution Guyot has been compared to that of the present-day Bahamas.
-
Vegetated island on Suwarrow
Water temperatures in the early
Through the history of the platform
Life on Resolution Guyot included
Uplift and karstification
During the Albian to Turonian (93.9 – 89.8 ± 0.3 million years ago[21]),[108] the carbonate platform rose above the sea by about 100 metres (330 ft)[109]–160 metres (520 ft). This uplift episode at Resolution Guyot is part of an episode of more general tectonic changes in the Pacific Ocean, with a general uplift of the ocean floor and tectonic stress changes at the ocean margins. This tectonic event has been explained by a major change in mantle convection in the middle Cretaceous pushing the ocean floor upward and sideward.[110]
When Resolution Guyot rose above sea level,
Drowning and post-drowning evolution
Resolution Guyot drowned either about 99 ± 2 million years ago[118] or during the Maastrichtian (72.1 ± 0.2 to 66 million years ago[21]),[47] although a hiatus in shallow carbonate deposition appears to date back to the Albian[112][119] that may reflect a long pause in deposition or increased erosion.[112] The end Albian period was characterized by widespread cessation of carbonate sedimentation across the western Pacific.[120][108] It is possible that carbonate sedimentation later continued until Campanian (83.6 ± 0.2 – 72.1 ± 0.2 million years ago[21])-Maastrichtian times.[71] The platform was certainly submerged by Pliocene (5.333 – 2.58 million years ago[21]) times.[11]
Other carbonate platforms in the Pacific drowned especially at the end of the Albian,
After the drowning, crusts formed by ferromanganese and by phosphate-modified rocks developed on exposed surfaces at Resolution Guyot.[20] Several different layers of phosphate modification have been observed during the Albian alone[119] and this process may have begun when the platform was still active; water within the rocks may have triggered phosphatization at this stage.[126] The ferromanganese deposition probably only began in the Turonian-Maastrichtian,[71] when the seamount had subsided to a sufficient depth.[127] Manganese-encrusted Cretaceous limestones have been found within the pelagic sediments.[128]
As at other guyots in the Pacific Ocean
Carbonates were dissolved and replaced by dolomite already during the Aptian and Albian. Around 24 million years ago at the Paleogene-Neogene (23.02 – 2.58 million years ago[21]) boundary, a second pulse of dolomite formation took place; perhaps sea level changes associated with global climate change triggered this second pulse.[97] The formation of the dolomites was probably aided by the fact that seawater can percolate through Resolution Guyot,[48] which may be responsible for the formation of fluid vent structures on the surface of the seamount.[132]
Notes
- drill cores from the oceans.[4]
- ^ Pit-like depressions within carbonate rocks that are filled with water.[32]
- ^ Cementation is a process during which grains in rock are solidified and pores filled by the deposition of minerals such as calcium carbonate.[54]
- ^ Volcanic rocks that appear as fragments.[69]
- ^ A makatea is a raised coral reef on an island, such as on Atiu, Mangaia, Mauke and Mitiaro in the Cook Islands.[115]
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