Hemigrapsus oregonensis
Hemigrapsus oregonensis is a small shore crab of the family Varunidae; formerly classified under the family Grapsidae. It is known under several common names, including yellow shore crab, hairy shore crab, green shore crab, mud-flat crab, bay shore crab and Oregon shore crab. Despite its common name, the crab actually has a wide variety of coloration. It is found along the West Coast of the United States and Canada, specifically along shorelines and similar geographical areas. In 2009, H. oregonensis was included on a list of animals petitioning for the endangered species label, but there was not enough scientific information available for it to be considered as such, so it remains unevaluated to the present day.
Description
This crab is an intertidal crab with wide-set eyes and no rostrum. Despite its name, body color can vary. Often, the crab's rectangular-shaped carapace is deep red or brown with light green spots, but it can also be grey-green, yellow-green, pale green or white with small blue/black spots, as well as have lighter colored legs with similar spots. The carapace in the hind region is free from transverse ridges, but contains three teeth between the orbit and lateral angle. The carapace typically measures 29.1 mm wide for female crabs and 34.7 mm wide for male crabs. Males and females can also be distinguished by the shape of their abdomens; females have more of an oval shape while males have a slightly pointed shape. The legs are covered in setae, and the legs with claws are tipped with white or yellow with no purple spots. The on the hind legs are unflattened.Habitat, distribution, and diet
The entire genus is restricted to the Pacific Ocean, except for Hemigrapsus affinis which lives along the Atlantic coasts of South America, from Cape San Roque to the Gulf of San Matías, and population of Hemigrapsus sanguineus which have been introduced from the species' native range in East Asia to the Atlantic coast of the United States from Portland, Maine to North Carolina, and to the English Channel and North Sea.This species typically lives under rocks in intertidal zones, but can also be found along shorelines, and in mud flats, algal mats, eelgrass beds and the tidal mouths of large rivers. It prefers areas with diverse plant matter, fine sediment and slow, protected currents. Its geographical range in the United States spans from Resurrection Bay to Bahía de Todos Santos. It is heavily concentrated in the San Francisco Bay, along the coasts of Oregon and Washington, and along the west coast of Canada, specifically in coastal British Columbia and on Vancouver Island.
Hemigrapsus oregonensis
Estelline Salt Spring
In 1962, Gordon C. Creel described a population of crabs in the Estelline Salt Springs, describing and naming them as Hemigrapsus estellinensis in 1964. The spring where it lived were contained by the United States Army Corps of Engineers. It differed from its relatives by the pattern of spots on its back, and by the relative sizes of its limbs, but genetic analysis in 2020 confirmed H. estellinensis as a junior synonym of H. orogenensis.Hemigrapsus estellinensis was described as having a rectangular carapace with almost parallel sides. Males have a carapace length of up to and a carapace width of up to, while females have a carapace up to long and wide. The front corners of the carapace are developed into three strong teeth on each side. The chief difference between H. estellinensis and other species in the genus is the extensive pattern of rust-red spots on the animal's "drab green" carapace. H. estellinensis also has a pair of conspicuous white spots near the ends of the H–shaped indentation on the animal's back, and another spot between each of those spots and the lateral margin of the carapace. The legs are marked with larger spots than the carapace, and both the chelipeds and the walking legs are shorter than in other species. There are no spots on the animal's underside, including the abdomen. In males, the chelipeds bear a hairy patch containing chemoreceptors on the ventral side of the claw. Creel collected 6 males and ten females; one of the males is the holotype and all the others are paratypes. All sixteen are held in the National Museum of Natural History as specimens USNM 107855 and USNM 107856. A few living specimens were taken to Wayland College, but died within 17 hours for unknown reasons. Two of the females laid eggs before dying, one laying 3,000 and the other 8,000.
H. estellinensis lived in Estelline Salt Springs east of the town of Estelline in Hall County, Texas, from the nearest ocean. Before its extinction, it was the only troglobitic crab in the contiguous United States. Its occurrence so far from the ocean has been described as "curious", and the species was "probably a Pleistocene relic".
The springs originally produced water with a salinity of 43‰ that fed the Prairie Dog Town Fork of the Red River. The salinity derives from Permian red beds, and has a strong structuring effect on the Red River's biota. It had a flow of approximately per minute, and the pool was wide at the surface, which was at an altitude of above sea level. At a depth of, it was only wide, and then widened slightly down to a depth of. Below that, an opening wide led into a cavern completely filled with water.
The United States Army Corps of Engineers built a dike around the Estelline Salt Springs in January 1964, which has reduced the chloride load on the Red River by per day. Before it was contained, the spring had a rich biota, comprising the cyanobacteria Oscillatoria and Lyngbya, the green algae Ulva clathrata and U. intestinalis, twenty species of diatom, many invertebrates – including a species of barnacle – and a single fish species, Cyprinodon rubrofluviatilis. The springs have since increased in salinity, and many species have been driven to extinction, including H. estellinensis and the undescribed barnacle. As early as December 1962, attempts to find further living individuals of H. estellinensis were unsuccessful, and it was probably extinct before Creel's description was published in 1964.