Page 62 - Introduction to Paleobiology and The Fossil Record
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FOSSILS IN TIME AND SPACE  49


                                                                              Craton
                                                                              boundary of Tethyan and Boreal
                                                                       J  J
                                                                              provinces in Jurassic
                                                                       T  T   boundary of high and middle
                                                                              paleolatitude faunas in
                             +                                         P  P  }
                   60          +                                              Triassic and Permian
                                      T  T  ?
                                                                       T  T   boundary of middle and low
                                                                              paleolatitude faunas in
                                                                             }
                                                                       P  P   Triassic and Permian
                                    +
                                           P  P
                                                                               Zone of displaced terranes
                   50                    +
                                                                              Tethyan faunas
                                              T  T  ?
                                              J  J                            Permian
                                                                              Triassic
                                                                              Jurassic (Pliensbachian)
                                                                              Boreal faunas
                                                                         +    Jurassic (Pliensbachian)
                   40





                                               P  P
                   30






                   20



             Figure 2.17  Displaced faunas in terranes within the North American Cordillera together with changing
             provincial boundaries on the craton. Postulated latitudinal boundaries on the craton during the
             Permian, Triassic and Jurassic are indicated and confirm the northern movement of these displaced

             terranes. A dataset of Jurassic ammonoid distributions across the cordilleran terranes is available at
             http://www.blackwellpublishing.com/paleobiology/. These data may be analyzed and manipulated using
             a range of multivariate techniques including cluster analysis (see also Hammer & Harper 2005). (From
             Hallam, A. 1986. J. Geol. Soc. 143.)




             Much more recently in central Scotland, reli-   ancient continents are often termed “suspect”.
             able early Ordovician dates from the High-      In many cases it is not clear to which if any
             land Border Complex (based on brachiopods,      of the continents they were originally attached.
             trilobites and a range of microfossils), previ-  The Highland Border Complex was consid-
             ously included as part of the mainly Neopro-    ered a truly suspect terrane. Moreover, the
             terozoic Dalradian Supergroup on the            two areas could not have developed together
             continent of Laurentia, suggests that these     since, fi rstly, during the Early Ordovician, the
             rocks were deposited in one of a series of      Dalradian was deforming and uplifting, and
             basins along the margin of Laurentia. The       secondly there was a lack of Dalradian clasts
             oceanic terranes, such as volcanic islands and   in the Highland Border Basin. Some scientists
             microcontinents, that evolved seaward of the    have even suggested the Dalradian was derived
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