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Pacific Northwest Coast - ScholarsArchive at Oregon State University

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Appendix 4E: Building a Benthic Habit<strong>at</strong> Model as Surrog<strong>at</strong>es<br />

for Ecosystem-Scale Targets<br />

This section describes the first steps in developing and comparing models for mapping offshore<br />

benthic habit<strong>at</strong>s in the <strong>Pacific</strong> <strong>Northwest</strong> <strong>Coast</strong> Ecoregion. This, like all benthic models, is a work<br />

in progress. We utilized a topographic model and existing classific<strong>at</strong>ions th<strong>at</strong> characterize depth<br />

and benthic substr<strong>at</strong>e to model and gener<strong>at</strong>e offshore benthic conserv<strong>at</strong>ion targets. Use of the<br />

benthic habit<strong>at</strong> model assumes th<strong>at</strong> benthic habit<strong>at</strong> types can serve as a surrog<strong>at</strong>e or coarse filter<br />

for the conserv<strong>at</strong>ion of the majority of bottom-dwelling species in an ecoregion. The ideal d<strong>at</strong>a for<br />

mapping marine ecosystems is biological d<strong>at</strong>a on the distribution and abundance of species in the<br />

w<strong>at</strong>er and on the sea bottom. Unfortun<strong>at</strong>ely, these d<strong>at</strong>a are scarce offshore.<br />

Lacking regionally comprehensive biological d<strong>at</strong>a along the <strong>Pacific</strong> <strong>Northwest</strong> <strong>Coast</strong> (PNWC), the<br />

Conservancy has focused on the use of geophysical d<strong>at</strong>a. We predict th<strong>at</strong> many geophysical<br />

variables (e.g., temper<strong>at</strong>ure, depth and sediment type) can be correl<strong>at</strong>ed with the occurrence of<br />

different types of species. Geophysical inform<strong>at</strong>ion th<strong>at</strong> is most useful includes sea surface<br />

temper<strong>at</strong>ure, bottom temper<strong>at</strong>ure, depth, bottom sediment type, phytoplankton density<br />

(chlorophyll a), currents and b<strong>at</strong>hymetry (underw<strong>at</strong>er topography). Our current model presented<br />

here uses b<strong>at</strong>hymetry and marine geology to depict depth, geomorphology or bedforms, and<br />

substr<strong>at</strong>e type.<br />

It is our hope th<strong>at</strong> the benthic model will be predictive of habit<strong>at</strong> targets. Output of the model,<br />

however, needs to be tested against higher resolution d<strong>at</strong>a (i.e., multibeam) and underw<strong>at</strong>er<br />

surveys to determine the accuracy of identifying landforms on the seafloor. In addition, these d<strong>at</strong>a<br />

need to be correl<strong>at</strong>ed with biotic assemblages in determining community or habit<strong>at</strong> types. A<br />

recent study used local popul<strong>at</strong>ion density estim<strong>at</strong>es of juvenile demersal finfish from trawl survey<br />

d<strong>at</strong>a as a meaningful indic<strong>at</strong>or of habit<strong>at</strong> value (Cook and Auster 2005). We believe associ<strong>at</strong>ing<br />

species d<strong>at</strong>a with modeled d<strong>at</strong>a on benthic habit<strong>at</strong>s will ultim<strong>at</strong>ely give us a more accur<strong>at</strong>e sp<strong>at</strong>ial<br />

assessment of species-habit<strong>at</strong> utiliz<strong>at</strong>ion. Lastly, it should be noted th<strong>at</strong> this model cannot be used<br />

to predict surface or w<strong>at</strong>er column p<strong>at</strong>terns in diversity. Other models are required in examining<br />

the pelagic environment.<br />

4E.1 Classific<strong>at</strong>ion of the Benthic Environment<br />

In order to gener<strong>at</strong>e a continuous surface depicting the seafloor we used a number of regional<br />

b<strong>at</strong>hymetric d<strong>at</strong>a sets and examined interpol<strong>at</strong>ion techniques. Digital Elev<strong>at</strong>ion Models (DEMs)<br />

of the seafloor are distinct from terrestrial models in th<strong>at</strong> the survey efforts required to produce a<br />

continuous surface of depth across a region are often inconsistent temporally, sp<strong>at</strong>ially and<br />

methodologically. Therefore careful examin<strong>at</strong>ion of interpol<strong>at</strong>ion methods was conducted before<br />

an appropri<strong>at</strong>e surface was used to model benthic habit<strong>at</strong>s.<br />

After gener<strong>at</strong>ing a continuous surface depicting the seafloor, we examined several models th<strong>at</strong><br />

classify the benthic environment into distinct geomorphic types. The benthic model presented<br />

here has been used for marine ecoregional planning throughout the continental U.S., including the<br />

Southern and Northern California ecoregions, the Floridian and Carolinian on the east coast, as<br />

well as in the <strong>Northwest</strong> Atlantic <strong>Coast</strong>al and Marine region. In addition to developing an initial<br />

methodology and d<strong>at</strong>a for depicting benthic habit<strong>at</strong>s we have also used the b<strong>at</strong>hymetric source d<strong>at</strong>a<br />

to determine areas of bottom complexity. Although using the same source d<strong>at</strong>a, output from a<br />

complexity model complements the identific<strong>at</strong>ion of benthic habit<strong>at</strong>s and therefore will be<br />

addressed separ<strong>at</strong>ely. Both methodologies were conducted along the outer coasts of <strong>Oregon</strong> and<br />

Washington, part of the <strong>Pacific</strong> <strong>Northwest</strong> <strong>Coast</strong> ecoregion (Figure 4E.3.1).<br />

The results of the benthic habit<strong>at</strong> model described below produce offshore marine conserv<strong>at</strong>ion<br />

targets. This approach to modeling coarse scale habit<strong>at</strong>s provides promise in areas of the world<br />

PNW <strong>Coast</strong> Ecoregional Assessment Appendix 4E, page 1 of 8

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