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Welcome to the 31st IUBS General Assembly and Conference on ...

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Swedish Museum of Natural His<str<strong>on</strong>g>to</str<strong>on</strong>g>ry, S<str<strong>on</strong>g>to</str<strong>on</strong>g>ckholm, Sweden. Email:<br />

christian.pott@nrm.se<br />

Plants with cycad‐like leaves (cycadophytes) played a key<br />

role in <str<strong>on</strong>g>the</str<strong>on</strong>g> Mesozoic vegetati<strong>on</strong> prior <str<strong>on</strong>g>to</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> late Mesozoic<br />

ecological radiati<strong>on</strong> of flowering plants. The Mesozoic,<br />

<str<strong>on</strong>g>the</str<strong>on</strong>g>refore, has sometimes been referred <str<strong>on</strong>g>to</str<strong>on</strong>g> as <str<strong>on</strong>g>the</str<strong>on</strong>g> ‘age of<br />

cycads’, but it has l<strong>on</strong>g been clear that <str<strong>on</strong>g>the</str<strong>on</strong>g>se cycadophyte<br />

leaves were produced by at least two groups of seed plants<br />

that were not closely related phylogenetically, i.e.<br />

Cycadales <str<strong>on</strong>g>and</str<strong>on</strong>g> Bennettitales. The Cycadales are a small<br />

group of extant plants that in most phylogenetic<br />

rec<strong>on</strong>structi<strong>on</strong>s are placed as <str<strong>on</strong>g>the</str<strong>on</strong>g> basal branch in <str<strong>on</strong>g>the</str<strong>on</strong>g> seed<br />

plant tree. The Bennettitales are in morphology‐based<br />

analyses usually placed with angiosperms, Gnetales,<br />

extinct Erdtmani<str<strong>on</strong>g>the</str<strong>on</strong>g>cales, <str<strong>on</strong>g>and</str<strong>on</strong>g> Pen<str<strong>on</strong>g>to</str<strong>on</strong>g>xylales in a<br />

m<strong>on</strong>ophyletic group (<str<strong>on</strong>g>the</str<strong>on</strong>g> anthophytes). Major problems<br />

with attempts <str<strong>on</strong>g>to</str<strong>on</strong>g> resolve seed plant phylogeny are<br />

extensive extincti<strong>on</strong>s <str<strong>on</strong>g>and</str<strong>on</strong>g> inadequate knowledge of <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

extinct groups; many fossil taxa included in<br />

morphology‐based analyses are in urgent need of<br />

re‐evaluati<strong>on</strong> using modern techniques <str<strong>on</strong>g>and</str<strong>on</strong>g><br />

rec<strong>on</strong>structi<strong>on</strong> <str<strong>on</strong>g>to</str<strong>on</strong>g>ols. Of particular interest is an improved<br />

underst<str<strong>on</strong>g>and</str<strong>on</strong>g>ing of <str<strong>on</strong>g>the</str<strong>on</strong>g> fossil taxa included in <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

anthophytes <str<strong>on</strong>g>and</str<strong>on</strong>g> o<str<strong>on</strong>g>the</str<strong>on</strong>g>r potentially related fossils. Recent<br />

studies show that <str<strong>on</strong>g>the</str<strong>on</strong>g> cycadophytes were more diverse<br />

than previously accepted <str<strong>on</strong>g>and</str<strong>on</strong>g> that <str<strong>on</strong>g>the</str<strong>on</strong>g> current<br />

classificati<strong>on</strong> of <str<strong>on</strong>g>the</str<strong>on</strong>g> group was oversimplified. At least 6<br />

distinguishable groups (fossil <str<strong>on</strong>g>and</str<strong>on</strong>g> modern Cycas‐like<br />

cycads, o<str<strong>on</strong>g>the</str<strong>on</strong>g>r modern cycads, Nilss<strong>on</strong>iales, Cycadeoidaceae,<br />

Williams<strong>on</strong>iaceae, Pen<str<strong>on</strong>g>to</str<strong>on</strong>g>xylales) are generally<br />

incorporated in <str<strong>on</strong>g>the</str<strong>on</strong>g> cycadophytes. These groups<br />

encompass diverse plant architectures, foliage types,<br />

reproductive architectures, <str<strong>on</strong>g>and</str<strong>on</strong>g> ecology, which deserve<br />

more detailed investigati<strong>on</strong>s <str<strong>on</strong>g>to</str<strong>on</strong>g> resolve <str<strong>on</strong>g>the</str<strong>on</strong>g>ir phylogenetic<br />

relati<strong>on</strong>ships <str<strong>on</strong>g>and</str<strong>on</strong>g> ecological preferences. The talk will<br />

give an overview of <str<strong>on</strong>g>the</str<strong>on</strong>g> status quo <str<strong>on</strong>g>and</str<strong>on</strong>g> analyse <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

challenges in cycadophyte tax<strong>on</strong>omy/nomenclature by<br />

means of selected examples.<br />

When <str<strong>on</strong>g>the</str<strong>on</strong>g> world turned ‘brown’: Resource<br />

competiti<strong>on</strong>, apparent competiti<strong>on</strong> <str<strong>on</strong>g>and</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

‘Miocene Transformati<strong>on</strong>’<br />

Yoram AYAL<br />

Ben Guri<strong>on</strong> University, PO Box 102 Midreshet Ben Guri<strong>on</strong>, Israel.<br />

Email: ayal@bgu.ac.il<br />

The Miocene was a key epoch during which <str<strong>on</strong>g>the</str<strong>on</strong>g> early<br />

Cenozoic, mostly forested, biomes were transferred <str<strong>on</strong>g>to</str<strong>on</strong>g><br />

<str<strong>on</strong>g>the</str<strong>on</strong>g> late Cenozoic–Quaternary, open forests <str<strong>on</strong>g>and</str<strong>on</strong>g><br />

grassl<str<strong>on</strong>g>and</str<strong>on</strong>g>s biomes. Current <str<strong>on</strong>g>the</str<strong>on</strong>g>ories suggest that this<br />

transformati<strong>on</strong> was due mainly <str<strong>on</strong>g>to</str<strong>on</strong>g> abiotic fac<str<strong>on</strong>g>to</str<strong>on</strong>g>rs,<br />

mainly <str<strong>on</strong>g>the</str<strong>on</strong>g> development of cooler <str<strong>on</strong>g>and</str<strong>on</strong>g> more seas<strong>on</strong>al<br />

climates, <str<strong>on</strong>g>and</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> decrease in CO 2 levels. Here I suggest<br />

an alternative, ecologically based, hypo<str<strong>on</strong>g>the</str<strong>on</strong>g>sis <str<strong>on</strong>g>to</str<strong>on</strong>g> explain<br />

<str<strong>on</strong>g>the</str<strong>on</strong>g> recorded changes in biomes structure.<br />

During <str<strong>on</strong>g>the</str<strong>on</strong>g> late Oligocene, some browsing mammals<br />

reached body‐size that enabled <str<strong>on</strong>g>the</str<strong>on</strong>g>m <str<strong>on</strong>g>to</str<strong>on</strong>g> minimize<br />

predati<strong>on</strong> pressure <strong>on</strong> <str<strong>on</strong>g>the</str<strong>on</strong>g>m <str<strong>on</strong>g>and</str<strong>on</strong>g> as a result <str<strong>on</strong>g>the</str<strong>on</strong>g>ir<br />

populati<strong>on</strong>s increased <str<strong>on</strong>g>to</str<strong>on</strong>g> a level where <str<strong>on</strong>g>the</str<strong>on</strong>g>y<br />

over‐browsed <str<strong>on</strong>g>the</str<strong>on</strong>g> forest trees <str<strong>on</strong>g>and</str<strong>on</strong>g> c<strong>on</strong>trol <str<strong>on</strong>g>the</str<strong>on</strong>g>m. Thus,<br />

many forested biomes changed <str<strong>on</strong>g>the</str<strong>on</strong>g>ir state from being<br />

‘green’ (where plants are resource limited) <str<strong>on</strong>g>to</str<strong>on</strong>g> ‘brown’<br />

(where plants are herbivore c<strong>on</strong>trolled). The<br />

competiti<strong>on</strong> for diminishing browser resources<br />

resulted in <str<strong>on</strong>g>the</str<strong>on</strong>g> evoluti<strong>on</strong> of diverse body‐plane of<br />

browsers enabling finer resource partiti<strong>on</strong> <str<strong>on</strong>g>and</str<strong>on</strong>g> high<br />

species diversity. The heavy browsing started <str<strong>on</strong>g>to</str<strong>on</strong>g> limit<br />

trees abundance, opening forest gaps <str<strong>on</strong>g>and</str<strong>on</strong>g> as a result,<br />

<str<strong>on</strong>g>the</str<strong>on</strong>g> spread of grassy areas within <str<strong>on</strong>g>the</str<strong>on</strong>g> forested <strong>on</strong>es. The<br />

spread of open forests selected for <str<strong>on</strong>g>the</str<strong>on</strong>g> evoluti<strong>on</strong> of<br />

mix‐feeding habitat generalist Proboscidea, <str<strong>on</strong>g>and</str<strong>on</strong>g><br />

open‐grassl<str<strong>on</strong>g>and</str<strong>on</strong>g> grazers. C<strong>on</strong>comitantly, <str<strong>on</strong>g>the</str<strong>on</strong>g> open forest<br />

<str<strong>on</strong>g>and</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> spreading grassl<str<strong>on</strong>g>and</str<strong>on</strong>g> gave advantage <str<strong>on</strong>g>to</str<strong>on</strong>g> habitat<br />

generalist Carnivora over <str<strong>on</strong>g>the</str<strong>on</strong>g> forest specialists<br />

Creod<strong>on</strong>ta. Thus, at <str<strong>on</strong>g>the</str<strong>on</strong>g> end of <str<strong>on</strong>g>the</str<strong>on</strong>g> Miocene <str<strong>on</strong>g>and</str<strong>on</strong>g> early<br />

Pliocene, habitat specialist titanic perissodactyle<br />

browsers were outcompeted by habitat generalist<br />

Proboscidea, <str<strong>on</strong>g>and</str<strong>on</strong>g> habitat generalist felids <str<strong>on</strong>g>and</str<strong>on</strong>g> canids<br />

replaced <str<strong>on</strong>g>the</str<strong>on</strong>g> forest specialist creod<strong>on</strong>ts. C<strong>on</strong>comitantly,<br />

apparent competiti<strong>on</strong> between (a) medium <str<strong>on</strong>g>to</str<strong>on</strong>g> large,<br />

grassl<str<strong>on</strong>g>and</str<strong>on</strong>g> grazers <str<strong>on</strong>g>and</str<strong>on</strong>g> forest browsers, through habitat<br />

generalist large felids <str<strong>on</strong>g>and</str<strong>on</strong>g> (b) grasses in <str<strong>on</strong>g>the</str<strong>on</strong>g> open forests<br />

<str<strong>on</strong>g>and</str<strong>on</strong>g> grassl<str<strong>on</strong>g>and</str<strong>on</strong>g>s <str<strong>on</strong>g>and</str<strong>on</strong>g> trees in <str<strong>on</strong>g>the</str<strong>on</strong>g> forested habitat through<br />

mix‐feeding Proboscidea, resulted in <str<strong>on</strong>g>the</str<strong>on</strong>g> extincti<strong>on</strong> of<br />

many of <str<strong>on</strong>g>the</str<strong>on</strong>g> forest‐dwelling browsers, <str<strong>on</strong>g>the</str<strong>on</strong>g> decline of <str<strong>on</strong>g>the</str<strong>on</strong>g><br />

forested biomes <str<strong>on</strong>g>and</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> spread of grassl<str<strong>on</strong>g>and</str<strong>on</strong>g>s.<br />

Workshop <strong>on</strong> investigative case­based<br />

learning<br />

Margaret WATERMAN <str<strong>on</strong>g>and</str<strong>on</strong>g> E<str<strong>on</strong>g>the</str<strong>on</strong>g>l STANLEY<br />

89

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