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choose to use any of those alternatives here if we wanted to, but we would still need to consider whether a given alternative was appropriate for our particular implementation. We need to use the JMS operations directly in any client (caller) code that wishes to communicate with the MDB instances. Therefore, we will always use some JMS operations directly whenever we choose to use the Remote Messaging facilities provided by the JMS platform. This is true regardless of whether we choose to use MDBs or a more direct JMS implementation approach within the callee s code. Although we can choose to implement the listener code directly in the callee, it is not recommended when the full J2EE platform is available for us to use. For this reason, our J2EESKIT implementation (which we will discuss in 17) does not use JMS calls. Also, because our JMS-SKIT does use the JMS operations, we choose to focus on the Remote-Code Execution in the J2EE-SKIT the J2EE-SKIT does not use MDBs. However, using JMS operations or MDBs in future projects based on the J2EE-SKIT is not forbidden or discouraged.

pal caveman ancestors are simply one more example of the many vertebrates (most famously bats) which shelter in caves, but hunt out in the open The importance of this type of cave dweller to the overall ecology of karst terrains cannot be overstated, for the activities of cavesheltering vertebrates effectively transfer nutrients from the photosynthetic world to the subsurface via the feeding defecation cycle A voluminous and steadily growing literature exists on the ecology of karst terrains, both above and below the water table (see Wilkens et al 2000 for an extensive review) Here we are concerned solely with groundwater ecology in karst terrains As in other groundwater ecosystems (cf Section 643), a specialist terminology has been developed to describe the subsurface af liations of different organisms Thus a troglobite is de ned as an organism which can only live in caves.

Thinking in the language of values unlocks powerful possibilities for growth and action, but at rst blush it can seem dangerous to some. For the senior management of companies, shifting the way you lead and govern people from rules-based to values-based thinking sometimes brings the fear of losing control. Governing by rules shifts less power down the hierarchy, allowing those at the top to believe they can easily control the actions of those below them. This is a habit of mind left over from the days of fortress capitalism and feudalism. Leading from values, on the other hand, decentralizes power and shifts the responsibility for decision making into the hands of individuals at all levels. Values are not black-and-white or quantitative. Values are like trust; they empower others to honor or betray you. They open up avenues of possibility and leave room for interpretation. Surprisingly, though, values-based leadership has a tremendous upside. As business units spread around the world and more and

Troglophiles are organisms which prefer the cave environment, but are able to ourish elsewhere if necessary Finally trogloxenes are essentially surface life-forms which use caves for shelter As in other subsurface ecosystems, the distributions of the various categories of organisms throughout karst terrains re ects the availability of various environmental resources Take a trip into a cave (preferably one not perpetually lighted for the bene t of tourists) and you will quickly appreciate how soon daylight is left behind Once you are past the reach of daylight, no more green plants will be present; the only ora will be the vari-colored microbial bio lms which are sporadically present on cave walls and ceilings With the loss of green plants, there is an abrupt decline in the availability of detrital organic carbon, which is an important source of nutrition for the microfauna.

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In the furthest recesses of the cave, atmospheric oxygen is usually also in short supply, and carbon dioxide may reach dangerously high concentrations (promise me you ll turn back before you reach that zone ) The relative isolation of many cave atmospheres from the surface means that cave environments tend to have far more stable climates than the overlying surface environment.