Anton Dohrn Seamount

Coordinates: 57°30′N 11°00′W / 57.500°N 11.000°W / 57.500; -11.000[1]
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Anton Dohrn Seamount
North Atlantic Ocean
Anton Dohrn Seamount is located in North Atlantic
Anton Dohrn Seamount
Summit depth600 metres
Height1,500 m
Location
Location
EEZ)
Geology
TypeGuyot
Last eruption~40 million years

The Anton Dohrn Seamount is a

Atlantic
. It is 1.8 kilometres (1.1 mi) high and is topped with pinnacles, one of which reaches a depth of 530 metres (1,740 ft). Away from the flat top upon which the pinnacles rest, the slopes fall off steeply into the Rockall Trough and a moat in the sediment that surrounds the seamount.

It appears to be a volcano formed by basaltic lava and tuff. It formed during the Cretaceous and Paleogene and was proposed to be a source for bentonite layers across the British Isles. After the Cretaceous, subsidence and erosion lowered its top until it sank below sea level. The seamount was discovered in 1958.

Anton Dohrn Seamount hosts a diverse ecosystem characterized by

xenophyophorans
, which themselves host a number of animals. It has been affected by human fishing operations, however.

Name and research history

Anton Dohrn Seamount is also known as Anton Dohrn Kuppe, a name used by German charts,[2] and as Anton Dohrn bank.[3] It was discovered on 22 September 1958 by the survey vessel Gauss during the Polarfront programme and later surveyed on 18–19 April 1959 by the fishery research vessel FFS Anton Dohrn.[4]

Geography and geomorphology

Anton Dohrn Seamount is located in the northeast

Rockall Trough, an over 2,000 metres (6,600 ft) deep submarine depression of unclear origin. North-northeast lies the Rosemary Bank and Hebrides Terrace Seamount is found south-southeast from the seamount.[6] The seamount is located inside the exclusive economic zone of the United Kingdom.[8]

Anton Dohrn Seamount is a 1.8 kilometres (1.1 mi) high[9] and about 45 kilometres (28 mi)[10]–40 kilometres (25 mi) wide circular[9] guyot[6] with a flat top at 1,100–530 metres (3,610–1,740 ft) depth.[11] Flat-topped seamounts are unusual in the North Atlantic.[12] The shallowest point of the seamount lies at about 530 metres (1,740 ft) depth[9] and is formed by a pinnacle that protrudes from the c. 600 metres (2,000 ft) deep summit platform.[10] A 100 metres (330 ft) thick layer of sediment covers the flat top[13] and appears to be reworked by storms and sea currents.[9] Mounds,[14] slope breaks and other volcanic pinnacles are located on the flat top.[15] The seamount tilts southeastward.[16]

Beyond the margin of the flat top, the slopes of Anton Dohrn Seamount drop down to 2,400 metres (7,900 ft) depth.[17] The steep slopes have been variously described as either lacking a sediment cover[1] or featuring gravelly sediments along with outcropping bedrock.[7] There are cliffs, ridges[11] and rockfalls[14] but no gullies or canyons.[8] Parasitic cones lie on the northwestern slope. A moat surrounds the seamount[15] and reaches depths of about 2,300 metres (7,500 ft).[10] It might have formed either through erosion of surrounding sediments by ocean currents or through isostatic subsidence.[18]

Geology

The

Iceland plume's buoyancy. The Iceland plume has uplifted terrain as far as 1,000 kilometres (620 mi) from the plume.[19] A 100 kilometres (62 mi) long crustal lineament known as the Anton Dohrn Lineament crosses through the seamount; it may extend into Scotland and Rockall Bank[20] and runs in northwest–southeast direction.[21]

Anton Dohrn Seamount is probably formed mostly by basaltic lava[10] and tuffs[12] which define a transitional to alkaline suite.[22] The rocks contain feldspar and olivine phenocrysts as well as plagioclase. They are covered with ferromanganese crusts[23] and vesicles contain carbonates, clay and zeolites which formed through alteration.[24] Chalks of Maastrichtian age,[23] Eocene nearshore conglomerates[25] and Miocene muds and sands have also been recovered.[26] A granite rock has been dredged as well; it may be a dropstone from icebergs[27] and such exotic rocks have been found in other dredge samples.[12]

Geologic history

Anton Dohrn Seamount is a former volcano.[9] Radiometric dating of volcanic rocks dredged from it has yielded ages of 70 ± 1, 62 ± 1, 47 ± 1 and 41 ± 1 million years ago,[28] indicating episodic activity over 29 million years.[9] Pulses of volcanic activity of similar age have been identified at other volcanoes in the region and may reflect fluctuations of the Iceland plume.[29] The onset of volcanic activity may have been the consequence of crustal extension in the region.[12] The activity during the Cretaceous implies that rifting in the North Atlantic was already underway at that time.[30] At that time, the Rockall Trough was at least 1 kilometre (0.62 mi) deep.[31]

phreatomagmatic eruptions that could have dispersed volcanic ash in the region.[32] This volcanic ash erupted by Anton Dohrn may be the source of post-Cenomanian bentonites of the British Isles[33] but the age and composition of the bentonites do not support this theory.[34] The seamount was once proposed to be the source of Turonian tephra deposits in Western Europe before its Maastrichtian age was established.[35]

During the Cretaceous the seamount was about 2 kilometres (1.2 mi) higher than present,[19] perhaps even reaching 2,000 metres (6,600 ft) height above sea level;[16] presumably it was then eroded during the Paleocene when a wave of erosion took place in western Britain and stripped much of the volcanic centres of northwest Scotland.[19] An episode of crustal subsidence in the Cretaceous-Oligocene also played a role in lowering Anton Dohrn Seamount.[36] The pinnacles on the seamount may be leftover volcanic conduits that resisted erosion.[12] Sedimentation covered the seamount and its flanks in the Eocene and continued afterwards.[9]

Ecology

bivalve Xylophaga anselli has been found at Anton Dohrn Seamount and the Hebrides slope.[41]

A number of ecosystems have been found on Anton Dohrn Seamount, including

soft corals like as Anthomastus sp. have also been found at parasitic vents.[7] The cold water coral cover can become so thick that the underground disappears underneath it.[49]

Synaphobranchus kaupi and squat lobsters Munida sp. have also been encountered.[45][50][51]

Seamounts are considered to be biodiversity hotspots,[52] and there are proposals to make Anton Dohrn Seamount a Special Area of Conservation.[8] The region is considered to be "the cradle of deep-sea biology" as Victorian-era scientists sampled the regional fauna.[8] Ocean currents around Anton Dohrn Seamount are complicated and formed by various water masses.[10] Internal tides at the seamount appear to be important for its ecosystem.[53]

The seamount has been impacted by

microplastics.[55] In October 2020 the seamount was made part of the West of Scotland Marine Protected Area by the Scottish Government in attempt to protect the area's ecology.[56][57]

References

  1. ^ a b c Jones et al. 1994, p. 239.
  2. ^ Rogalla 1962, p. 60.
  3. ISBN 978-1-4613-3487-3
    .
  4. ^ Rogalla 1962, p. 59.
  5. ^ Stewart et al. 2009, p. 10.
  6. ^ a b c d Jones et al. 1994, p. 238.
  7. ^ a b c Stewart et al. 2009, p. 9.
  8. ^
    ISSN 1726-4170
    .
  9. ^ a b c d e f g Stewart et al. 2009, p. 12.
  10. ^ a b c d e Davies et al. 2015, p. 4.
  11. ^ a b Stewart et al. 2009, p. 31.
  12. ^ a b c d e Jones et al. 1974, p. 129.
  13. ^ Jones et al. 1994, p. 244.
  14. ^ a b Stewart et al. 2009, p. 34.
  15. ^ a b Stewart et al. 2009, p. 14.
  16. ^ a b Jones et al. 1974, p. 130.
  17. ^ Stewart et al. 2009, p. 130.
  18. ISSN 1616-7228
    .
  19. ^ a b c Jones et al. 1994, p. 245.
  20. S2CID 135171946
    .
  21. S2CID 133667534
    .
  22. ISSN 0025-3227
    .
  23. ^ a b Jones et al. 1994, p. 240.
  24. ^ Jones et al. 1994, p. 241.
  25. ^ Stoker, Weering & Svaerdborg 2001, p. 411.
  26. ^ Stoker, Weering & Svaerdborg 2001, p. 431.
  27. ^ Rogalla 1962, p. 62.
  28. ^ O'Connor et al. 2000, p. 955.
  29. ^ O'Connor et al. 2000, p. 957.
  30. ISSN 0016-7878
    .
  31. ISSN 2053-5910
    .
  32. ^ Pacey 1984, p. 57.
  33. ^ Pacey 1984, p. 58.
  34. S2CID 130913700
    .
  35. ISSN 0044-0604
    .
  36. ^ Jones et al. 1974, pp. 130–131.
  37. ^ Stewart et al. 2009, p. 13.
  38. S2CID 85606978
    .
  39. ISSN 2053-5910
    .
  40. S2CID 83864961
    .
  41. PMID 25061913
    .
  42. ^ Davies et al. 2015, pp. 14–15.
  43. ^ a b Henry et al. 2014, p. 1.
  44. ^ Davies et al. 2015, p. 24.
  45. ^ a b Stewart et al. 2009, pp. 38–46.
  46. ^ Davies et al. 2015, p. 16.
  47. ^ Davies et al. 2015, pp. 26–27.
  48. ISSN 1054-3139
    .
  49. ^ Stewart et al. 2009, p. 30.
  50. ^ Davies et al. 2015, pp. 12–13.
  51. ISSN 0012-821X
    .
  52. ^ Davies et al. 2015, p. 2.
  53. ^ Henry et al. 2014, p. 5.
  54. ^ Stewart et al. 2009, p. 74.
  55. S2CID 3355997. Archived from the original
    (PDF) on March 5, 2020. Retrieved March 15, 2020.
  56. ^ "Europe's largest marine protected area comes into force". BBC News. October 9, 2020. Retrieved October 23, 2020.
  57. ^ "West of Scotland Marine Protected Area". Joint Nature Conservation Committee. Retrieved October 23, 2019.

Sources

External links
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