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Marine Resources Assessment for the Marianas Operating ... - SPREP

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AUGUST 2005 FINAL REPORT<br />

In<strong>for</strong>mation Specific to <strong>the</strong> <strong>Marianas</strong> MRA Study Area—The expected occurrence <strong>for</strong> endangered marine<br />

mammals is based primarily on <strong>the</strong> occurrence of <strong>the</strong> sperm whale but <strong>the</strong> humpback whale’s occurrence<br />

patterns were also considered. Throughout <strong>the</strong> year, endangered marine mammals in <strong>the</strong> <strong>Marianas</strong> MRA<br />

study area are expected to occur seaward of <strong>the</strong> shelf break into open ocean waters (Figure B-2). This is<br />

based on expected occurrence of <strong>the</strong> sperm whale in this area. There is a low or unknown occurrence of<br />

endangered marine mammals from <strong>the</strong> coastline (excluding harbors and coastlines) to <strong>the</strong> shelf break,<br />

except during June through September when <strong>the</strong>re is no possible occurrence of endangered marine<br />

mammals (specifically, <strong>the</strong> humpback whale) in lagoons (Figure B-2).<br />

♦ North Pacific Right Whale (Eubalaena japonica)<br />

Description—Until recently, right whales in <strong>the</strong> North Atlantic and North Pacific were classified<br />

toge<strong>the</strong>r as a single species, referred to as <strong>the</strong> “nor<strong>the</strong>rn right whale.” Genetic data indicate that <strong>the</strong>se<br />

two populations represent separate species: <strong>the</strong> North Atlantic right whale (Eubalaena glacialis) and<br />

<strong>the</strong> North Pacific right whale (Eubalaena japonica) (Rosenbaum et al. 2000).<br />

Right whales have a robust body shape; overall body color is black, although many individuals also<br />

have irregular white patches on <strong>the</strong>ir undersides (Reeves and Kenney 2003). There is no dorsal fin<br />

on <strong>the</strong> broad back. The largest recorded North Pacific right whales are an 18.3 m female and a 16.4<br />

m male (Omura et al. 1969); North Pacific right whales are larger than <strong>the</strong>ir North Atlantic<br />

counterparts (Reeves and Kenney 2003). The head is nearly one-third of <strong>the</strong> total body length. The<br />

jawline is arched and <strong>the</strong> upper jaw is very narrow in dorsal view. The head is covered with irregular<br />

whitish patches called “callosities,” which have whale lice attached.<br />

Status—The North Pacific right whale is perhaps <strong>the</strong> world’s most endangered large whale species<br />

(Perry et al. 1999; IWC 2001). North Pacific right whales are classified as endangered both under <strong>the</strong><br />

ESA and on <strong>the</strong> IUCN Red List (Reeves et al. 2003). There are insufficient genetic or resighting data<br />

to address whe<strong>the</strong>r <strong>the</strong>re is support <strong>for</strong> <strong>the</strong> traditional separation into eastern and western stocks<br />

(Brownell et al. 2001); however, Clapham et al. (2004) noted that north-south migratory movements<br />

support <strong>the</strong> hypo<strong>the</strong>sis of two largely discrete populations of right whales in <strong>the</strong> eastern and western<br />

North Pacific. No reliable population estimate presently exists <strong>for</strong> this species; <strong>the</strong> population in <strong>the</strong><br />

eastern North Pacific is considered to be very small, perhaps only in <strong>the</strong> tens of animals (NMFS 2002;<br />

Clapham et al. 2004), while in <strong>the</strong> western North Pacific, <strong>the</strong> population may number at least in <strong>the</strong><br />

low hundreds (Brownell et al. 2001; Clapham et al. 2004). There is no designated critical habitat <strong>for</strong><br />

<strong>the</strong> North Pacific right whale (NMFS 2002).<br />

Habitat Preferences—Feeding habitat <strong>for</strong> right whales is defined by <strong>the</strong> presence of sufficiently high<br />

densities of prey, especially calanoid copepods (Reeves and Kenney 2003). Development of those<br />

patches is essentially a function of oceanic conditions, such as SST, stratification, bottom topography,<br />

and currents, which concentrate zooplankton, and concentration is probably enhanced by <strong>the</strong><br />

behavior of <strong>the</strong> organisms <strong>the</strong>mselves (Beardsley et al. 1996; Tynan et al. 2001). The shift in Bering<br />

Sea right whale occurrences from deep waters in <strong>the</strong> mid-twentieth century to <strong>the</strong> mid-shelf region in<br />

<strong>the</strong> late 1900s was attributed to changes in <strong>the</strong> availability of optimal zooplankton patches, possibility<br />

relating to climatic <strong>for</strong>cing (variability in oceanic conditions caused by changes in atmospheric<br />

patterns) (Tynan et al. 2001). Sightings in <strong>the</strong> Bering Sea are clustered in relatively shallow water<br />

(waters with a bottom depth of 50 to 80 m) (Tynan et al. 2001). However, North Pacific right whales<br />

also have been sighted in waters with bottom depths as deep as 1,700 m (Carretta et al. 1994). The<br />

IWC (2001) noted a surprising absence of evidence <strong>for</strong> coastal calving grounds, since right whales in<br />

<strong>the</strong> North Atlantic and in <strong>the</strong> Sou<strong>the</strong>rn Hemisphere have calving grounds located in shallow bays,<br />

lagoons, or in waters over <strong>the</strong> continental shelf.<br />

Distribution—Right whales occur in sub-polar to temperate waters. The North Pacific right whale<br />

historically occurred across <strong>the</strong> Pacific Ocean north of 35°N, with concentrations in <strong>the</strong> Gulf of Alaska,<br />

eastern Aleutian Islands, south-central Bering Sea, Sea of Okhotsk, and <strong>the</strong> Sea of Japan (Omura et<br />

al. 1969; Scarff 1986; Clapham et al. 2004). Presently, sightings are extremely rare, occurring<br />

primarily in <strong>the</strong> Okhotsk Sea and <strong>the</strong> eastern Bering Sea (Brownell et al. 2001). Prior to 1996, right<br />

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