Horseshoe crabs in Australia

                   Bull Edu Shizuoka Univ Nat Sci 53 (2003)

 

 

   When you watch the title of “Horseshoe crabs in Australia", you may think that there are horseshoe crabs in Australia now.  However, there are not any horseshoe crabs in the Australia zone including Australia now. This report is the story of horsesoe crabs  which had been used to live in Australia and were found as fossils.

   On  the  other  hand,  three species of horseshoe crabs now live in east south  Asia,  that  is,  the  Oriental zone.  The boundary of the Oriental  zone  and  the  Australia zone is the Wallace's line or the Weber's  line.  The  Wallace's line situates at the west of the Sulawasi (Celebes)  island,  and the  Weber's line situates at the east of the same  island.  There   is   a  report that a species of horseshoe crab,  Tachypleus  tridentatus  lives in the Sulawasi island (Sekiguchi, 1988).   Therefore in future, we may find some living horseshoe crabs in natural condition at north west Australia.

   There   are   now   four  species  of  horseshoe crabs in the world.  Limulus   polyphemus   lives  in  the east  coast of north America  continent.   Other  three  species  live in Asia continent. Tachypleus  tridentatus  lives in  Japan, south China, north Vietnam and islands of east  south  Asia.   T.  gigas  lives the area of Asia continent from south Vietnam  to  east  India  and  the  islands  of east  south   Asia.   Carcinoscorpius  rotundicauda  lives  the area of  Asia  continent from south China to east India and the islands of east  south  Asia.  We can  notice  those  three Asian species live in the Oriental zone except Japan. 

   The ancester of all  four species is seemed to be the same species called Mesolimulus walchi which inhabited in Europe 200 million years ago.

   There are only four species of horseshoe crabs in the present world, but there used to be many species of horseshoe crabs in the whole world. In  Australia,  there  were  many  horseshoe crabs.  Almost of those horseshoe  crabs in  Australia lived in fresh water.  We are surprised in this fact,   because all present horseshoe crabs live in sea water or brackish water.

   We  visited to Australia in 2001 and could get the informations about  fossils  of horseshoe crabs there.  We now report you about the rise and fall of Australian horseshoe crabs.

   More than 200 milion years ago, all continents were gathered into only one land in the earth.  Australia was face to the south pole continent and India and close to Africa continent.  At the time, Australia was situated at the higher latitude than present one.  We call the gathered land Pangaea. As there is a ocean call Tethys Sea, Pangaea was divided into two parts.  We call  the north  part Laurasia continent or Angara continent, and the south part Gondwana continent.

   Mesolimulus walchi used to inhabit in the Europe which was in Laurasia continent,  therefore  we  can  regard they inhabit on the north coast of Tethys sea.   The  horseshoe  crabs, which moved toward west, became Limulus  polyphemus  and  another  horseshoe crabs, migrated toward east, became Asian  horseshoe crabs.  We  can suppose to think the horseshoe crabs came into  India  after  when  the Indian subcontinent hit the Laurasia and became one land the Eurasian continent.

   At 600 million ago, the beginning of the Paleozoic era, the very  strong  living  organism  appeared  and  prospered.   That  is trilobites  (【Subphylum】 Trilobitomorpha).  The  trilobites became extinct at the end of the Paleozoic era, 230 million ago.   On the other hand, its direct descendant 【Subphylum】 Chelicerata including horseshoe crabs  still  have  survived   until the present, somehow.  Horseshoe crabs  seem  to have been  evolved  from   【Order】  Redlichiida  in trilobites  at  the  first period of the  Paleozoic era.  Somebody say  horseshoe crabs evolved  from  【Suborder】  Redichia  of  【Order】 Redlichiida in trirobites,  but  we  can  see  more similarity with Olenellus vermontanus  of 【Suborder】 Olenellia in same 【Order】 Redlichiida .

   The famous sea scorpions (【Class】 Eurypteria) are also relative with horseshoe crabs.  Both   animals belong to 【Subphylum】 Chelicerata.  One kind of sea scorpions reached the land and was evolved into land scorpions and spiders, that is, 【Class】 Arachnida. 

   Both  trilobites  and sea scorpions inhabited widely but they became exinct in the Paleozoic era.  Only the horseshoe crabs have still alive in the  present  sea  among  Trilobitomorpha  and   marine Chelicerata. Consequently, we should protect horseshoe crabs.

   The process of evolution such as the evolvement from 【Subphylum】 Trilobitomorpha  to 【Subphylum】  Chelicerata,  the appearance of 【Class】 Xiphosura and the appearance of 【Order】 Xiphosurida seem to occur in Laurasia continent according to fossil unearthing.  When we call horseshoe crabs in paleontology, it stands for the species of 【Order】 Xiphosurida.  So that 【Order】  Aglaspida  in same 【Class】 Xiphosura is not called horseshoe crabs (Table 1).

   Most fossils of horseshoe crabs and its relatives are definitely found in Laurasia continents and very a few of those fossils are found in Gondwana continent including Australia.  Only five kinds of fossil horseshoe crabs have been reported in Australia.  However, it is certain that horseshoe crabs used to inhabit in Australia.

   The  oldest fossil horseshoe crabs in Australia are Kasibelinurus amicorum, founded in the stratum of late Devonian period, 400 million to 350 million years old.  The word Kasibelinurus means a company of Belinulus. Belinulus is the horseshoe crab founded in Europe and it means tails such as the  arrow.   The   word  amicorum means friendly.  The length of Kasibelinurus  amicorum fossile is 63 mm  and it was founded at near the Parkes in New South Wales (Fig. 1; Pickett 1993).  As it was founded at the sea layers, it is likely to be saltwater horseshoe crabs.  To ours interests, other horseshoe crabs in Australia were  found in the fresh water  strata.   There  are reports of the fossil horseshoe crabs as the same  genus  as  Kasibelinurus  species  in  Europe and North America continents so that the genus widely spread in the earth.

Fig.1. Kasibelinurus amicorum. The figure was written by Pickett (1993), and the photograph was taken by us at Australian museum.

   Kasibelinurus belongs to 【Suborder】 Limulina. There are some opinions in relation  with  the belong 【Family】.  We feel it can belong to 【Family】 Paleolimulidae,  but Pickett (1933) made it belongs to the new 【Family】 Kasibelinurus.  We can not agree to make many 【Family】.  It is very difficult.  We think the horseshoe  crabs  of  the  Paleozoic era are classified  into  【Family】  Paleolimulidae except the species belonging to 【Suborder】 Synziphosurina, and ones of the Mesozoic era into 【Family】 Mesolimulidae,  and  ones of the Cenozoic era including the present ones into 【Family】 Limulidae.  That is, there are only three families.

   There is a same problem about 【Superfamily】.  We think 【Superfamily】 is not needed.  Somebody think 【Superfamily】 Belinuracea and 【Superfamily】 Euproopacea.  However, we can not feel that there is big differences between Belinuracea, Euproopacea and Paleolimulidae, so that it is unnecessary for them to divide many 【Superfamily】.  We propose Belinurus and Euproops should belong to 【Family】 Paleolimulidae in 【Suborder】 Limulina.

   We  can see the body segments of 【Suborder】 Synziphosurina have been  independent and each segments work individually.  On the other hand, the  segments  of  【Suborder】  Limulina fuse.  The segments of 【Family】 Paleolimulidae is clear in spite of fuse.

   The fossil of Synziphosurina, similar to Kasibelinurus, has founded from the  strata  of  early  stage  of  Devonian period in Bolivia of south America  (Eldredge,  1974).  This Bolivian fossil has been recorded as the oldest horseshoe crab in Gondowana continent.  The theory of that the evolutionary  process from 【Suborder】 Synziphosurina to 【Suborder】 Limulina happened in Laurasia continent, is strong possibility but we can not deny that the process might have happened in Gondowana continent.

   An  Aglapida  fossil has found  from the strata of the late Cambrian period  in  the  early Paleozoic era at north Tasmania, Australia (Jago and Baillie,  1992).  Aglaspida  is not horseshoe crabs, but it is close order of Xiphosurida, that is, horseshoe crabs (Table 1).
   A fossil, Hemiaspis tunnecliffei has found from the strata of Silurian period and another fossil, Pincombella belomontensis has founded from the strata  of  late Permian period.  Both species were reported as horseshoe crabs  by  Chapman  (1932).    However,  as the result of detailed investigation, it elucidated that Hemiaspis tunnecliffei was a species of trilobites and Pincombella belomontensis was an insect (Pickett, 1984).

   The  fossil,  certainly  judged  as  a horseshoe crab, is a Paleolimulidae  which  has  founded  from  the strata of the late Permian period in Poatina in Tasmania island (Fig. 2, Ewington etal., 1989).  It located between 75 to 80  degrees north latitude and suppose to be cold climate at the time.  And the fossils has found from the strata, made from  fresh  water, so that the horseshoe crabs suppose to be fresh water horseshoe crabs.  The length is 3 cm, except for tail telson.

Fig.2. The horseshoe crab fossil of Paleolimulidae from Tasmania. From Ewington & Banks (1989).

   Horseshoe crabs, born in Paleozoic era, lived over the last Paleozoic era which trilobites came exinct and also horseshoe crabs inhabit during the period of dinosaurs, Mesozoic era.  Horseshoe crabs in Australia also lived over the time of extinct at the end of Paleozoic era.  

   The  fossil  of  Dubbolimulus  peetae  has been found  from the strata  of the  middle  Triassic  period  of Mesozoic era at Dubbo in New South Wales (Fig, 3, Pickett, 1984).  As it is a horseshoe crab in  Mesozoic   era,   it  is   possible   to  belong  to  the 【Family】 Mesolimulidae, but  Pickett (1984)  proposed  it  belongs  to new 【Family】  Dubbolimulidae.  Surely we can see the wide prosoma which is  peculiar   to   Australian    horseshoe   crabs,  on  the Dubbolimulus.  Dubbolimulus   lived  in  flesh  water.   The total length  is  4 cm, width of prosoma is 27.8 mm, and the length of prosoma is 14.0 mm.  

Fig.3. Dubbolimulus peetae. The figure was written by Pickett (1984), and the photograph was taken by us at Australian museum.

   An astonishing, symbolic Australian fossil horseshoe crab was found from the 200 million years old strata of Beacon hill at Brookvale of Sydney in New South  Wales.  It is Austrolimulus fletcheri (Fig. 4, Rick, 1955, 1968). It may belong to 【Family】 Mesolimulidae, but Rick (1955, 1968) has proposed new 【Family】 Austrolimulus.  You can see the figure widens remarkably.  Two fossils have found and the bigger one's total length is 14.6 cm, the length excluding  telson is 5.7 cm.  The width is 17.8 cm.  You can recognize the width is longer than the length.  There is no stings on the abdomens and telson  is  longer than the body.  This symbolic Australian horseshoe crab also lived in fresh water.

Fig.4. Austrolimulus fletcheri. The photograph was gotten at Australian museum.

   The last horseshoe crab in Australia has found from the strata of early Cretacean period at Koonwarra in Victoria. It is Victalimulus mcqueeni (Fig. 5, Rick and Gill, 1971).  This horseshoe crab is the latest one in Australia.  Cretaceous is the last period of Mesozoic era and the wild extinction happened and dinosaurs also became exinct at the time.  Although Australian horseshoe crabs lived over the last Paleozoic era, they seemed not to be able to live over the last Mesozoic era and they became extint in the same  way  as dinosaurs.  This Victalimulus also found from the strata of  fresh water so that they seem to have lived in fresh water.  However, Rick  and  Gill (1971) mentioned it might have lived in salt water or brackish  water,  considering that there are stratas of salt water near there.  If the conjecture was true, it became to think that they had gone into the river or  lake  and became a fossil after millions years.  This Victalimulus looks like Mesolimulus walchi which lived in Europe before 200 millions years and the  ancestor of present horseshoe crabs.  We think it should be studied more about the origin of Victalimulus.

Fig.5. Victalimulus mcqueeni. From Riek & Gill (1971).

   Mesolimulus  walchi  found from strata of salt water and the four kinds of living horseshoe crabs are all living in salt water.  But, They prefer weak salt water than strong salt water, nevertheless there is a record of Carcinoscorpius rotundicauda was found in the river which is 150 km far from the river mouth.  Limulus polyphemus vitaly live in near 50% sea water. 

   After all, Australian horseshoe crabs are said to all became extinct at the  end of Mesozoic era, but we expect that living horseshoe crabs in fresh  water might still exist in some rivers or lakes of Australia, because Australia is the mysterious continent.

 

 

 

Acknowledgement     

 

We deeply thank Dr. Robert Jones and staffs' cooperation in Sydney Museum, staffs of Seahorse Museum, and Dr. Karen Gowlett-Holms and staffs of Eagle Howk  Diver  Center.  We would like to express our heartfelt thanks to Dr. Chip Clark of Smisonian Museum in Washington D.C.

 

 

 

References

 

Andel, T.H.V. (1985)  New views on an old planet. Continental drift and the     history of the earth.  Cambridge Univ. Press, Cambridge.     

Bcardman, R.S. (1987)  Fossil Invertebrates.  British Library, London.

Chapman, F. (1932)  Two new Australian fossil king-crabs.  Proc. R. Soc.      Vict. n.s. 44, 100-102.

Eldredge, N. (1974)  Revision of the suborder Synziphosurina (Chelicerata,      Merostomata), with remarks on merostome phylogeny.  Am. Mus. Novit.       2543, 1-41.

Eldredge, N. (1991)  Fossils.  Harry N. Abrams, INC., New York.

Ewington, D.L., Clarke, M.J. & Banks, M.R. (1989)  A late Permian fossil       horseshoe crab (Paleolimulus: Xiphosura) from Poatina, Creat Weatern       Tiers, Tasmania.  Pap. Proc. R. Soc. Tasm. 123, 127-131.

Itow, T. (1991)  Complex Biology.  Sugiyama Shoten, Tokyo.

Itow, T. (2001)  Facts which the world of sea and life teach to human beings.    Science House, Tokyo.

Jago, J.B. & Baillie, P.W. (1992)  An Idamean aglaspidid from northern        Tasmania.  Alcheringa 16, 14.

Moore, R.C. (1973)  Treatise on Invertebrate Paleontology, (P) Arthropoda 2.

   Geological Society of America & University of Kansas Press, Colorado.

Moore, R.C. (1977)  Treatise on Invertebrate Paleontology, (O) Arthropoda 1.

   Geological Society of America & University of Kansas Press, Colorado.

Pickett, J.W. (1984)  A new freshwater Limuloid from the middle Triassic of     New South Wales.  Palaeontology 27, 607-621.

Pickett, J. (1993)  A late Devonian xiphosuran from near Parkes, New South      Wales.  Mem.Ass.Australas. Palaeontols 15, 279-287.

Riek, E.F. (1955)  A new xiphosuran from the Triassic sediments at Brookvale,    New South Wales.  Rec. Austr. Mus. 23, 281-282. 

Riek, E.F. (1968)  A re-examination of two arthropod species from the        Triassic of Brookvale, New South Wales.  Rec. Austr. Mus. 27, 313-321.

Riek, E.F. & Gill, E.D. (1971)  A new xiphosuran genus from lower Cretaceous     freshwater sediments at Koonwarra, Victria, Australia.  Palaeontology      14, 206-210.

Sekiguchi, K. (ed.) (1988)  Biology of horseshoe crabs.  Science House,       Tokyo.