This post is one in a series of posts which compares the
depositional environment of the late Jurassic lithographic limestones at
Solnhofen in Germany based on extracts from Solnhofen: A Study in Mesozoic Palaeontology
with observations made at modern
intertidal mudflats at Ha Pak Nai, Deep Bay, New Territories; Yi O on Lantau and Luk Geng in the New Territories, Hong Kong and
proposes an intertidal mudflat origin for the examples cited.
This post compares references
to the presence of juvenile
horseshoe crabs found at Solhofen - Eichstatt with photographs of juvenile
horseshoe crabs in their natural habitat on three intertidal mudflats in Hong Kong.
Extract from: Solnhofen: A Study in
Mesozoic Palaeontology
Species: Mesolimulus
walchi
“… the juvenile horseshoe crab, Mesolimulus
and the crustacean Mecochirus were still alive for a short time on the lagoon
floor.” (Barthel et al - Page 58).
“The individuals which
crawled and died on the plattenkalk sediment in the Solnhofen- Eichstatt area
are all juveniles” (Barthel et
al - Pages 77 & 79).
“Almost all fossil
limulids from the western area of Solnhofen and Eichstatt are thought to be juveniles” (Barthel et al - Page
140).
Comments on
juvenile horseshoe crab habitats and ecology in Hong Kong
There are four species of horseshoe
crab living today, Limulus polyphemus,Tachypleus
tridentatus, Tachypleus gigas and
Carcinoscorpius rotundicauda. L.
polyphemus occurs along the east
coast of the USA and Mexico. The other three species occur in South-East Asia. T. tridentatus and C. rotundicauda occur in Hong Kong.
Each
of the living species of horseshoe crabs has different habitat requirements during
their lives, related to spawning, juvenile development and adulthood.
In
all living horseshoe crab species, spawning takes place on the high tide mark. After
spawning, eggs take up to 45 days to develop. Once hatched, small trilobite
larvae are released and according to the species, these develop in the spawning
area, or very close to it.
About one year after hatching, small juveniles
move to a nursery area in the intertidal zone, where they will spend up to
sixteen years, according to species, feeding and growing, regularly moulting as
they grow in size. Depending on the species, they may moult up to eighteen times
before reaching maturity (Sekiguchi.1988).
In Hong Kong those nursery areas are on
open intertidal mudflats, often associated with seagrass beds in the case of T. tridentatus and in and around
mangroves in the case of C. rotundicauda.
The juveniles of these two species in Hong Kong also appear to have
preferences for substrate type in their intertidal areas where they forage.
Intertidal mudflats in Hong Kong can be broadly categorized
as intertidal mudflats with a predominant sand component and intertidal
mudflats with a predominant mud component.This is important in understanding juvenile horseshoe crab
ecology because in Hong Kong juvenile T.
tridentatus favour intertidal mudflats with a high sand component, whilst
juvenile C. rotundicauda favour
intertidal mudflats with a high mud component
In addition, because of these preferences, whilst juveniles
of these two species occur sympiatrically at a number of locations, their
differing spawning and juvenile habitat requirements suggest their substrate
foraging preferences mean they do not directly compete with each other.
Photographs of juvenile horseshoe crabs and their habitats
in Hong Kong
Intertidal mudflat at Ha Pak Nai, with Halophila beccari seagrass beds
Juvenile T. tridentatus foraging trail on intertidal mudflat at Ha Pak Nai
Series of T. tridentatus juvenile moults collected at Ha Pak Nai in 2009
Photograph showing the size range of the juvenile moults collected at Ha Pak Nai in 2009
Intertidal mudflats with juvenile C. rotundicauda
Yi O, Lantau
Luk Geng, New Territories
References
Barthel, K.W., Swinburne, N.H.M., and Conway Morris, S. (1994).
Solnhofen: A Study in Mesozoic Palaeontology. Cambridge University
Press, Cambridge.
Sekiguchi. K. (1988). Biology of Horseshoe Crabs. Science
House Co., Ltd, Tokyo
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