Wednesday, January 23, 2013

Juvenile horseshoe crab behaviour – marginal spine marks

This post documents the behaviour of juvenile horseshoe crabs (Tachypleus tridentatus) based on observations made at an inter-tidal mudflat at Ha Pak Nai, Deep Bay, New Territories, Hong Kong.

All observable juvenile horseshoe crab activity on the mudflat appears to be synchronized with the tides. When the tide comes in, the juveniles bury themselves in the substrate. When the tide recedes, they emerge to forage.

In terms of juvenile horseshoe crab locomotion, two principal types of locomotion are observed – foraging in the substrate and walking on the substrate. This post covers both foraging and walking activity, which result in marginal spine impressions being left in the substrate.










Juvenile horseshoe crab behaviour – tail (telson) marks

This post documents the behaviour of juvenile horseshoe crabs (Tachypleus tridentatus) based on observations made at an inter-tidal mudflat at Ha Pak Nai, Deep Bay, New Territories, Hong Kong.

All observable juvenile horseshoe crab activity on the mudflat appears to be synchronized with the tides. When the tide comes in, the juveniles bury themselves in the substrate. When the tide recedes, they emerge to forage.

In terms of juvenile horseshoe crab locomotion, two principal types of locomotion are observed – foraging in the substrate and walking on the substrate. This post covers both foraging and walking activity, which result in tail mark impressions being left in the substrate.

An examination of many of these marks highlights the importance of the tail (telson) in navigation, showing how the tail is used in changing direction and turning.








Even a juvenile (1.5 cm prosoma width) with a reduced tail can leave a substantial tail mark, highlighting the important role the tail has in turning. See below:



Images to highlight the role of the tail in turning. See below: 


Saturday, January 5, 2013

Juvenile horseshoe crab behaviour - foraging

This post documents the behaviour of juvenile horseshoe crabs (Tachypleus tridentatus) based on observations made at an inter-tidal mudflat at Ha Pak Nai, Deep Bay, New Territories, Hong Kong.

All observable juvenile horseshoe crab activity on the mudflat appears to be synchronized with the tides. Before the tide comes in, the juveniles bury themselves in the substrate. When the tide recedes, they emerge to forage.

In terms of horseshoe crab locomotion, two principal types of locomotion are observed – foraging in the substrate and walking on the substrate. This post covers foraging activity.

Prosoma used like a “snow plough”

Juveniles forage at different depths in the sediment. These are photographs of various foraging juveniles. Observations suggest that some of the prosoma design and ornamentation on juveniles is used to reduce surface tension and separate the sediment that is being foraged through.






Spiral foraging trails

These are the spiral trails left as a result of foraging activity. Such “disoriented” trails constitute normal behavior and are the norm, not the exception!














Thursday, January 3, 2013

Understanding horseshoe crab palaeoecology

There are four species of horseshoe crab living today:

(a)    Limulus polyphemus;  
(b)   Tachypleus tridentatus;
(c)    Tachypleus gigas; and
(d)   Carcinoscorpius rotundicauda.

Limulus occurs along the east coast of the USA and Mexico. The other three species occur in South-East Asia.

Horseshoe crab ecology

Horseshoe crabs have specific and specialized habitat requirements at different stages of their lives, related to:
(a)     spawning;
(b)    juvenile development; and
(c)    adulthood.

These factors, particularly the habitat requirements for juvenile development are critical to understanding the palaeoenvironments in which horseshoe crab fossils are found.

Spawning habitats and early development

All four species of horseshoe crab have specific spawning requirements related to a combination of factors including tides, substrate type and sand grain size.

L. polyphemus, T. gigas and T. tridentatus usually nest on the high tide mark of protected sandy beaches, and each of these species appears to have very specific preferences as to range of sand grain size for nesting.

Unlike the three other species, C. rotundicauda, which is the smaller species, does not spawn on sandy beaches. Instead, it lays its eggs in subsurface, muddy substrate in streams, rivers or mangrove stands (C. rotundicauda has a different lifestyle to the three species above and this will be discussed in a separate blog post with specific reference to the palaeoenvironment of the Carboniferous Mazon Creek deposits)..

In areas where suitable beaches are not available, or have been diminished, L. polyphemus has been observed to lay eggs within the sediments of offshore sandbars that parallel beaches, in the vicinity of the deltas of tidal creeks or on the sandy banks of tidal marsh creeks.

Adult female horseshoe crabs carry thousands of eggs in a breeding season, which are laid in small batches over a period of time. Spawning is tied to the lunar cycles, taking place on high tides, so that the eggs can be laid specifically in the high tide zone, where it appears the correct microclimate involving a combination of temperature, moisture and oxygen content is critical to successful embryonic development and hatching (Brockman 2003).

Photographs

Spawning habitat - inside the spawning area

Development inside the egg


After spawning, embryonic development starts. Eggs take up to 45 days to develop.
(Image courtesy: City University, Hong Kong)

Development of trilobite larvae - inside the spawning area


Once hatched, small trilobite larvae are released, and according to the species, these develop in the spawning area, or very close to it. The two rows of images on the right are newly hatched 1st and 2nd instar trilobite larvae.
(Image courtesy: City University, Hong Kong)

Juvenile development habitat - on a "nursery beach"


About one year after hatching, trilobite larvae of the three large species move to a nursery beach in the inter-tidal zone, which is usually a shallow water mudflat in close proximity to the spawning site, where they will spend up to sixteen years as juveniles, feeding, growing and regularly moulting as they grow in size. This is the horseshoe crab nursery in seagrass beds (Halophila beccari) at Ha Pak Nai, Deep Bay, Hong Kong. The juveniles forage and develop in the pools between the seagrass mounds.


This is a series of juvenile Tachypleus tridentatus moults collected from the high tide lines at Ha Pak Nai in 2009 (the largest moult is 12.5 centimetres across the prosoma and represents the last stage of juvenile development).  Depending on the species, juvenile horseshoe crabs may moult up to eighteen times before reaching maturity (Sekiguchi 1988).

Adult habitat - on the seabed



After reaching maturity, the young adults move into deeper water to forage and grow. This is a mating pair of  adult Tachypleus tridentatus captured in the stream mouth at Ha Pak Nai in 2009. The larger female is on the left side of the photograph.

References

Brockman, H. J., (2003). Nesting behavior: A shoreline phenomenon. In: Shuster CN, Barlow RB, Brockman HJ, (Eds). The American Horseshoe Crab. Harvard University Press. Cambridge.

Sekiguchi. K. (1988). Biology of Horseshoe Crabs. Science House Co., Ltd, Tokyo.


Comparing fossil gastropod trails found at Solnhofen with gastropod trails found on the surface of a recent inter-tidal mudflat in Hong Kong

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 a modern inter-tidal mudflat at Ha Pak Nai, Deep Bay, New Territories, Hong Kong and proposes an inter-tidal mudflat origin for the examples cited.

This post compares comments on, and a photograph of trails made by the gastropod Rissoa sp. found at Solnhofen with photographs of foraging gastropods on the surface of the inter-tidal mudflats at Ha Pak Nai, Deep Bay, Hong Kong.

Extract from: Solnhofen: A Study in Mesozoic Palaeontology

“Also known are shorter, irregular trails made by the gastropod Rissoa, which may be very numerous in places, particularly Pfalzpaint, where the trails came from one or two beds. Rissoa may have lived on strands of algae which were also carried into the lagoon marooning their passengers” (Barthel et al - Page 79).


Photographs of gastropods foraging at Ha Pak Nai

(Scale where shown: 30 centimetre/12 inch ruler)

Littorina sp - small size gastropod




Batillaria sp - medium size gastropod





Small and medium size foraging trails together.
(the lower photograph is a close-up of the top photograph)





References

Barthel, K.W., Swinburne, N.H.M., and Conway Morris, S. (1994). Solnhofen: A Study in Mesozoic Palaeontology. Cambridge University Press, Cambridge.



Comparing fossil seaweed (attached to a rock anchor) found at Solnhofen with similar seaweed found along the coast at a recent inter-tidal mudflat in Hong Kong

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 a modern inter-tidal mudflat at Ha Pak Nai, Deep Bay, New Territories, Hong Kong and proposes an inter-tidal mudflat origin for the examples cited.

This post compares a photograph of a seaweed attaching to a rock as an anchor (Phyllothallus latifrons) found at Solnhofen with a series of photographs of a similar modern seaweed found along the coast of the inter-tidal mudflats at Ha Pak Nai, Deep Bay, Hong Kong, which seasonally wash up in large numbers in April and May each year.

Extract from: Solnhofen: A Study in Mesozoic Palaeontology

“The specimen shown in fig 7.1 is attached to a piece of reef rock similar to the reefal limestone which occurs to the south of Solnhofen in the region of Neuburg an der Donau” (Barthel et al - Page 103).


Photographs of seaweed attached to rocks and shells at Ha Pak Nai

(Scale where shown: 30 centimetre/12 inch ruler)

May 2009




April 2010



April 2011







References

Barthel, K.W., Swinburne, N.H.M., and Conway Morris, S. (1994). Solnhofen: A Study in Mesozoic Palaeontology. Cambridge University Press, Cambridge.