Antalo Limestone

Coordinates: 13°35′52″N 39°16′38″E / 13.5977°N 39.2772°E / 13.5977; 39.2772
Source: Wikipedia, the free encyclopedia.
Antalo Limestone
Ma
Approximate paleocoordinates
7°30′S 26°36′E / 7.5°S 26.6°E / -7.5; 26.6
RegionTigray
Country Ethiopia
 Eritrea
ExtentMekelle Outlier, Danakil Alps
Type section
Named forAntalo town
Named byWilliam Thomas Blanford
Year defined1868

The Antalo Limestone, also known as the Antalo Sequence, is a

fossiliferous limestones and marls that were deposited in a reef. Marine microfossils have shown an age between 165 and 150 million years.[1][2]

Name and definition

The Antalo Supersequence includes two main stratigraphic units: the Antalo Sequence and the Agula Group.

British Expedition to Abyssinia in 1868.[4] At that time, Hintalo was a major town on the route of the invading British army.[5] So far the nomenclature has not been proposed for recognition to the International Commission on Stratigraphy
.

Geographical extent

The sedimentary succession is found in Ethiopia, in the

Harrar Plateau and around Dire Dawa.[2]

Stratigraphic context

The Antalo Limestone overlies the Adigrat Sandstone, and is covered by the Agula Group or Agula Shale and the Mugher Mudstone.

Environment

The Antalo Limestone comprises sediment that was deposited in a shallow tropical sea in the

upper Jurassic. As the region had undergone a marine transgression, it was below the sea level. At that time, what would become Ethiopia was positioned just south of the equator.[6]

Lithology

Dogu’a Tembien

The limestones and

lagoons; (3) micritic (very fine grained) limestone with intercalations of wackestone and coquina beds deposited in relatively deep water; and (4) a succession of marls and limestone, with cherty limestone at the base.[2][3]

Addi Idaga
Miheno

Fossil content

Azef

The Antalo Limestone sediments were deposited at the time of dinosaurs and primitive birds. Well away from coasts, coral reefs formed the edge of the continental shelf. At shallow depth, the sea bottom was made of large

gastropods were common. There was also fish. As it was not a nutrient-rich ecosystem, larger predators were rare, maybe some marine reptiles like crocodiles. A striking scavenger in this fauna was a cephalopod mollusc, a giant nautilus with a characteristic spiral shell.[6]

Invertebrates

Bivalves
Bivalves of the Antalo Limestone.[7]
Genus Species Presence Material Notes Images
Actinostreon A. solitarium 10 specimens from AL1, 65 from AL2. 75 specimens. A palaeolophid.
Arcomytilus A. laitmairensis AL1 and AL2. 3 left valves, 1 right valve and 4 articulated specimens. A mytilid.
Eopecten E. velatus AL1. 1 left valve. A
pectinid
.
Gryphaea G.? (Bilobissa?) balli AL1. 1 left valve. A gryphaeid.
Integricardium I. (Integricardium) cf. bannesianum 7 specimens from AL1, 1 from AL2. 4 left valves, 1 right valves and 3 double-valved specimens. A
cardiid
.
Liostrea L. sp. AL1 and AL2. 2 specimens. An ostreid.
"Lucina" "L." cf. cecchii AL2. 4 double-valved specimens. A lucinid.
Modiolus M. (Modiolus) imbricatus 2 specimens from AL1, 1 from AL2. 3 double-valved specimens. A mytilid.
Musculus M. (Musculus) somaliensis AL1 and AL2. 2 articulated specimens. A mytilid.
Nanogyra N. nana AL2. 2 articulated specimens. A gryphaeid.
Pholadomya P. (Bucardiomya) somaliensis 1 specimen from AL1, 6 from AL2. 7 double-valved specimens. A pholadomyid.
P. (Bucardiomya) lirata AL2. 1 double-valved specimen. A pholadomyid.
Plagiostoma P. harronis AL1 and AL2. 3 left valves, 5 right valves and 2 articulated specimens. A limid.
P. sublaeviusculum AL2. 1 left valve 1 right valve and 1 articulated specimen. A limid.
Seebachia S. ("Eoseebachia") sowerbyana AL2. 2 left valves. An astartid.
Spondylopecten S. (Spondylopecten) palinurus AL1. 2 left valves. A
pectinid
.
Stegoconcha S. gmuelleri AL2. 2 articulated specimens. A pinnid.
Brachiopods
Brachiopods of the Antalo Limestone[7]
Genus Species Presence Material Notes Images
cf. Amydroptychus cf. A. sp. Base of AL2. 10 individuals. A rhynchonellid.
Cererithyris C. sp. 1 from AL1, 105 from AL2 . 106 individuals. A terebratulid.
Cymatorhynchia C. sp. AL2. 16 individuals. A rhynchonellid.
Daghanirhynchia D. sp. 3 individuals from AL1, 51 from AL2. 54 individuals. A rhynchonellid.
Monsardithyris M. sp. AL2. 20 individuals. A terebratulid.
Somalirhynchia S. africana Mostly from AL2. More than 100 individuals. A rhynchonellid.
Cnidarian
Cnidarians of the Antalo Limestone[7]
Genus Species Presence Material Notes Images
Actinastrea A. crassoramosa 47 specimens from AL1, 13 from AL2. 60 larger fragments of colonies. A
stony coral
.
Coenastraea C. arabica AL2. 1 specimen. A
stony coral
.
Collignonastraea C. cf. grossouvrei AL2. 1 specimen. A
stony coral
.
Columnocoenia C. gemmans AL1. 2 specimens. A
stony coral
.
Comoseris C. meandrinoides AL3. 1 complete colony. A
stony coral
.
Cladophyllia C. excelsa AL3. 1 specimen. A
stony coral
.
Cryptocoenia C. slovenica 7 specimens from AL1, 4 specimens from AL2. 11 specimens. A
stony coral
.
Ironella I. arabica AL1. 12 specimens. A
stony coral
.
Isastrea I. bernensis 20 specimens from AL1, 22 specimens from AL2. 42 specimens. A
stony coral
.
Kobyastraea K. lomontiana AL1. 1 specimen. A
stony coral
.
Latiastrea L. greppini 2 from AL1, 3 from AL2. 5 specimens. A
stony coral
.
Lochmaeosmilia L. trapeziformis AL1. 16 karger fragments of colonies. A
stony coral
.
Ovalastrea O. michelini AL2. 3 specimens (including 1 complete colony). A
stony coral
.
Echinoderms
Echinoderms of the Antalo Limestone
Genus Species Presence Material Notes Images
Ausichicrinites A. zelenskyyi Nearly complete specimen.[8] A comatulid.
Pygurus P. meslei Upper part of the formation.[9] A sea urchin.
Molluscs
Molluscs of the Antalo Limestone[10]
Genus Species Presence Material Notes Images
Orthosphinctes O. aff. tiziani Top part of sub-unit II. 5 fragmentary specimens. An
ammonite
.
Pachyceras P. cf. lalandeanum From the middle part of sub-unit II, GPS location 10°02′39.7″N, 38°13′53.7″E. One poorly preserved specimen (no. AF020). A
ammonite
.
Paracenoceras P. cf. ennianus Top part of sub-unit II. 1 specimen (no. AF012). A nautiloid.
P. aff. prohexagonum Lower Limestone Member.[11] A nautiloid.
P. cf. kumagunense Top part of sub-unit II. 1 specimen (no. AF004). A nautiloid.
P. cf. giganteum Middle part of sub-unit II. 1 specimen (no. AF005). A nautiloid.
Purpuroidea P. aff. gigas One specimen (AF025) from the top part of sub-unit I; One specimen (AF026) from the top part of sub-unit II. 2 specimen (AF025 and AF026). A gastropod.

Limestone and karst geomorphology

Santarfa

The layering is sub-horizontal, the same as that of the underlying sedimentary formations.

Traditional uses of Antalo Limestone

Dogu’a Tembien

Given its nearly rectangular shape and its strength, the hard layers of Antalo Limestone are used for

See also

References

  1. .
  2. ^ a b c d Bosellini, A.; Russo, A.; Fantozzi, P.L.; Assefa, G.; Tadesse, S. (1997). "The Mesozoic succession of the Mekelle Outlier (Tigrai Province, Ethiopia)". Mem. Sci. Geol. 49: 95–116.
  3. ^
    S2CID 199102740
    .
  4. ^ Blanford, W.T. (1870). Observations on the geology and zoology of Abyssinia, made during the progress of the British expedition to that country in 1867-68. London: Macmillan and Co.
  5. ^ Markham, C.; Prideaux, W. (1869). A history of the Abyssinian expedition. Macmillan.
  6. ^ .
  7. ^ .
  8. .
  9. .
  10. .
  11. .
  12. ^ Catlin, D; Largen, M; Monod, T; Morton, W (1973). "The caves of Ethiopia". Transactions of the Cave Research Group of Great Britain. 15: 107–168.
  13. ^ Nixon-Darcus, L.A. (2014). The cultural context of food grinding equipment in Northern Ethiopia: an ethnoarchaeological approach. PhD thesis. Canada: Simon Frazer University.
  14. ^ Gebre Teklu (2012). Ethnoarchaeological study of grind stones at Lakia'a in Adwa, Tigray Regional State, Ethiopia. PhD diss (PDF). Addis Ababa University.