It has long been known that children learning English optionally omit finite forms of the verb <em>be</em> (both copula and auxiliary). What makes <em>be</em> omissions possible? A classic answer is that <em>be</em> is semantically empty, hence a good choice to omit under performance-related pressures. What would this hypothesis lead us to expect about the infinitive form of <em>be</em>? In terms of semantic vacuity, nonfinite <em>be</em> is an even better choice for omission than finite <em>be</em> , since it does not carry tense or agreement information—most such deletions would be completely recoverable. Thus, the <em>semantic vacuity hypothesis</em> would lead us to expect omission of nonfinite <em>be</em> to be at least as frequent as omission of finite <em>be</em> . This is contrasted with the suggestion that <em>be</em> omission be incorporated into the Root/Optional Infinitive phenomenon. The latter <em>finiteness hypothesis</em> makes different predictions from the semantic vacuity hypothesis with respect to the relative rate of nonfinite <em>be</em> omission. The finding is that, in each relevant transcript, omission of finite <em>be</em> is attested, use of nonfinite <em>be</em> is attested, but there are no instances of omission of nonfinite <em>be</em> , contra the prediction of the semantic vacuity hypothesis. I develop an analysis within the Agreement/Tense Omission Model of the underspecification of Infl (cf. Schütze 1997). I claim that finite forms of <em>be</em> in (adult and child) English are <em>fused</em> V+I heads, in the sense of Halle & Marantz’s (1993) Distributed Morphology. Their locus for vocabulary insertion has values for person/number, tense, and lexical category. The fused vocabulary items cannot be inserted in a syntactic structure in which INFL features have been underspecified. Overt <em>be</em> arises only when both AgrS and Tense are fully specified. Null <em>be</em> , i.e. Ø, the default member of the paradigm, arises from underspecification of Tense and/or underspecification of AgrS.