Accessibility Skip to Global Navigation Skip to Local Navigation Skip to Content Skip to Search Skip to Site Map Menu

Geological dates and evolutionary rates: using river vicariance to pinpoint the pace of molecular change

Principle Investigator

Dr Jon Waters, Department of Zoology, University of Otago, New Zealand

Associate Investigators

Dr Chris Burridge, Department of Zoology, University of Otago, New Zealand
Assoc Prof Graham Wallis, Department of Zoology, University of Otago, New Zealand
Prof Dave Craw, Department of Geology, University of Otago, New Zealand
Prof Richard Norris, Department of Geology, University of Otago, New Zealand 

Background

DNA "clocks" provide an important method for determining time-scales of evolution. But the pace at which these clocks "tick" can be difficult to measure, particularly because DNA evolves at different rates in different species, and because rates may perhaps vary over time ("time-dependency"). Up until now, DNA clocks have been calibrated using ages of fossils, island formation, and a range of dated geological events (e.g. rise of the Panama Isthmus). But each of these methods potentially lacks precision for a variety of reasons. Our Marsden-funded research program seeks to establish calibrations across a range of geological ages using a new, more precise method: river evolution.

New Zealand's South Island is a geologically-dynamic and mountainous region that has experienced extensive glaciation and ongoing uplift (Fig 1) over several millions of years. This isolated, active landscape represents a natural laboratory for evolutionary research. Recent geological studies have revealed dramatic evolutionary histories for many South Island river systems. These histories include river reversal and river capture events— driven by tectonics and glaciation — that involve wholesale transfer of streams from one catchment to another (Fig 2). Examples of such drainage alterations are illustrated in Fig 3 (red arrows = present drainage; blue arrows = historic flow direction). In addition to their geomorphological effects, each of these geological changes has physically isolated populations of freshwater fish that were previously connected (vicariance) (Fig 2).

Fig. 1

Fig. 2

Research program

Our genetic studies indicate that river capture is one of the key factors underlying the biogeography and evolution of New Zealand’s freshwater fishes (Fig 4). The links we have discovered between river history and fish biogeography are analogous to a host-parasite system, with rivers as "hosts" and fish as "parasites". Under this model, river evolution can lead to the formation of new fish species. In simple terms, geological isolation leads to the accumulation of genetic differences among the separated fish populations. In addition, the amount of genetic divergence among populations is correlated with the length of geological isolation. Our project ultimately uses this causal link between geology and genetics to quantify rates of DNA change.

The importance of drainage history is particularly evident in New Zealand's far south, where the Nevis (Fig 3, red arrow 3; Fig 5) and Von (Fig 3, red arrow 8) have undergone dramatic reversals in flow. Galaxiid fish of the Von and Nevis rivers are genetically related to Southland populations (Fig 6: yellow circles) —rather than Clutha River populations (Fig 6: green circles) —consistent with historic rather than modern-day river connections (Fig 3).

Genetic relationships determined from mtDNA indicate strong recent links between Von River (Fig 7: dark blue haplotypes) and Southland populations of two different galaxiid species (G. gollumoides; G. 'southern'; Fig 7), as predicted from geological data. Importantly, the finding that this phylogeographic pattern is repeated across multiple species attests to its general significance.

Although much of our recent work has focussed on evolution in the rivers of southern South Island (see above), the situation is comparable further north. The waterways of central New Zealand, in particular, have similarly been shaped by recent glacial and tectonic activity (Fig 8). Analysis of river terraces in the Marlborough region indicates that the Pelorus River (Fig 8: arrow 9) once drained south through the Kaituna valley (Fig 8: arrow 5; Fig 9) into the Wairau River. Reversal of the Kaituna (Fig 8: arrow 5) led to isolation of these rivers and their associated fish populations. Based on geological dating techniques, we have developed a timeline for the isolation of these three river populations (Fig 10). We subsequently tested the geological hypothesis using fish collected from across the region (Fig 11).

DNA analysis of freshwater fish native to the Pelorus, Kaituna, and Wairau rivers has revealed genetic relationships (Fig 12) consistent with initial geological predictions (Fig 10). It is also clear that geological forces have produced parallel evolutionary effects on two unrelated fish species (Fig 12). Molecular clock calibrations derived from this interdisciplinary work imply that fish mtDNA is evolving substantially more rapidly than traditionally assumed.

Fig 2

Fig. 3

Fig 4

Fig. 4

Fig 5

Fig 5

Fig 6

Fig 6

Fig 7

Fig 7

Fig 8

Fig 8

Fig 9

Fig 9

Fig 11

Fig 11

Fig 12

Fig 12

Glaciation has yielded similar evolutionary consequences elsewhere in central New Zealand. In particular, geological data indicate that glacial connections between headwaters of the Clarence and Wairau rivers (Fig 13: arrow) ceased only 10-20,000 years ago. Under this model, we predicted that fish populations from the Clarence and Wairau systems would be closely related relative to geographically intermediate Awatere River populations (Fig 13). To assess this idea, we collected fish from all three systems (Fig 14). Subsequent DNA analysis strongly supported the geological model of late Pleistocene connectivity across the Clarence-Wairau divide. Specifically, Wairau and Clarence populations of both Galaxias 'northern' (Fig 15) and G. divergens (Fig 16) are closely related, whereas Awatere River populations of these species are, by contrast, distantly related (Fig 15, Fig 16).

Fig 13

Fig 14

Fig 15

Fig 16

Fig 17

Fig 18

As well as the congruent phylogenetic relationships paralleled across two distinct species, Wairau versus Clarence populations show almost identical levels of genetic differentiation in each case (Fig. 17). This increases our confidence that the link between geology and genetics is robust. In keeping with our results from a variety of independent studies, we can conclude that the galaxiid mtDNA clock is ticking substantially faster than expected.

Broader implications of this work

Our work has illustrated the important role of geology in shaping biological evolution, and thus shows the value of interdisciplinary approaches to evolutionary science. Biogeographical research certainly benefits from the predictive framework provided by geological information. Additionally, once a molecular clock is well-calibrated, genetic research can potentially be used to assess rates of landscape evolution. We anticipate that ongoing biological research will help to refine our understanding of geomorphology. In light of this genetic work involving several fish species, and spanning a broad range of geological events and timeframes, we are evaluating the "time-dependency" hypothesis recently suggested for vertebrate DNA evolution. This hypothesis predicts fast genetic divergence rates over short evolutionary timescales, but slower rates for older events. Our research certainly seems to support rapid rates of mtDNA change over short timescales, and we are beginning to assess the possible decay in rates over time (Fig. 18). If it finds widespread support, "time-dependency" will have major implications for our understanding of rates and causes of evolution, particularly over late Pleistocene and Holocene timescales.

More information

Waters, J.M. Rowe, D.L., Apte S., King, T.M., Wallis, G.P., Anderson, L., Norris, R.J., Craw, D., and Burridge, C.P. Geological dates and molecular rates: rapid divergence of rivers and their biotas. Systematic Biology 57:271-282 (2007)

Burridge, C.P., Craw, D., and Waters, J.M. An empirical test of freshwater vicariance via river capture. Molecular Ecology 16:1883-1895 (2007)

Craw, D., and Waters, J.M. Geological and biological evidence for regional drainage reversal during lateral tectonic transport, Marlborough, New Zealand. Journal of the Geological Society (in press)

Craw, D., Burridge, C., Anderson L. and Waters, J.M. Late Quaternary river drainage and fish coevolution, Southland, New Zealand. Geomorphology 84:98-110 (2007)

Craw D., Anderson, L., Rieser, U. and Waters, J. Drainage reorientation in Marlborough Sounds, New Zealand, during the last interglacial. New Zealand Journal of Geology and Geophysics 50:13-20 (2007)

Burridge, C.P., Craw, D., and Waters, J.M. River capture, range expansion, and cladogenesis: the genetic signature of freshwater vicariance.Evolution 60:1038-1049 (2006)

Waters, J.M., Allibone, R.M. and Wallis, G.P. Geological subsidence, river capture, and cladogenesis of galaxiid fish lineages in central New Zealand .Biological Journal of the Linnean Society 88:367-376 (2006)

Waters, J.M., Craw, D., Youngson, J.H. and Wallis, G.P. Genes meet geology: fish phylogeographic pattern reflects ancient, rather than modern, drainage connections. Evolution 55:1844-1851 (2001)