Red Rock Crab in the Coos Estuary
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The population of red rock crab appears stable in the Coos estuary but more data are needed to understand the population dynamics of this species.
Summary:
Red rock crabs do not burrow and tend to avoid sandy substrates as they lack any straining apparatus for sand removal (Rudy et al. 2013). They have been found at Crown and Collver Points in South Slough (deRivera et al. 2005) as well as the inner boat basin in Charleston (S. Groth, pers. comm., 2013). deRivera et al. (2005) found the highest numbers of red rock crabs closest to the mouth of the South Slough and found them conspicuously absent at their Winchester Creek and Sengstacken Arm study sites in the upper South Slough estuary, possibly due to lack of suitable habitat (Figure 2).
Red rock crabs are often found at the rocky dredge spoils areas north of Pigeon Point, in the greater Coos bay (Daly 1981) and have been found as far up the Coos estuary as McCullough Bridge in North Bend, even in wintertime when they prefer to stay in the deeper, more saline water (S. Groth, pers. comm., 2013). Because red rock crabs are osmoconformers whose body fluids match surrounding sea water salinity, they cannot tolerate brackish or fresh water for any length of time (Carroll and Winn 1989). Consequently, red rock crab distribution is influenced by tidally-driven salt water concentrations and are thus more commonly found in lower regions of the bay in times of large freshwater input (i.e., winter) and further up the bay during dryer periods (Daly 1981). During periods of high salinity in the upper estuary, red rock crabs outcompete both Hemigrapsus shore crab species for prime intertidal habitat (Daly 1981).
An inventory of the abundance and spatial distribution of red rock crabs in the Coos estuary would be very useful to better understand this ecologically important species.