2005 - Whitby Naturalists

2005 - Whitby Naturalists 2005 - Whitby Naturalists

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gafden in slcights, where radpoles remaincd undeveloped al1 summer aod .,,-,t until October did a few of them develop itrto frogs. I can offcr no explanation and know of no precedent for ti-ris; perhaps anothcr mernber can help. I hope X can persuade more mernbers t1; repolt sightings of rcptile s and rrnphibio. I am sure therc must hre rnorc than one newt in North Yorkshire! If reporteC sightings Co incrcase ilcxt ye;ir (ptreasc make an effort!) it will nct mean that mrmbers of animals have necessari-ly increased but it wili be interesting to l1ote the hahitars of varicrus com"mon creiltures anri important to notc any disastcrs as weti as reccrding the existence of ;rny rarities. SUE EVANS

THE GEOLOGICAL RECORDER'S REPORT Nodules And All That The grey nodules (morc properly called concretions) that we find sticking out of the Jurassic clifrs that buttress Whitby are often rhc source of our best fossils. If we look up at the sea cliffs we can see bands of thesc oval grey shapes running alorig the exposure. These nclduie beds must extend some distancc inland, for they formed on the floor o{ the vanished Tethys Ocean in the da-vs before the Atlantic and North Sca were rwinkles in the Earth's eye. Thc Tethys was a wann sea, for it once occupied that part of the globe whcre the Indian Ocean now sits: the continents which bordered the Tcthys have also brokcn up and re-formed into what we have today. Somc scraps of the Tethys rcm:lin; The Black Sea, The Caspian and the Aral Sca are all said to be remnants. But I wander ofr the pointl Concretions build when elements set free by thc decay of organic matter react rvith minerals in the deposited mud of the sea floor. Layers of new compounds grow .slowly around the organic 'seed'. The 'seed' may be a chunky ammonite or a group of trny molluscs or a mere scrap of she1l and flesh. Usually it is the hydrogen sulphide set free from decaying proteins which, by reacting with free ferric ions in the warer, begin to form thc concretion. The nodule will continue to grow until the right chemistry is availablc. Eventually that layer of seafloor will be buried and subjecred to pressurc. Fossils which havc not given rise to nodule growth will be crushed flat whilst those fossils within nodules are protected because of the great hardness of the concretion. Cliff erosion drops them onttl the shore; the sea wears thenr down and brcaks them open so that we find thcrn in various statcs of decay scattered around our feet; we pick thcm up, tum ttrem over and over and may notice the trace of a fossil. They are heavy because they are rich in Iron Pyrites. Strike them with a hammer and you might smell LO

gafden in slcights, where radpoles remaincd undeveloped al1 summer<br />

aod .,,-,t until October did a few of them develop itrto frogs. I can offcr<br />

no explanation and know of no precedent for ti-ris; perhaps anothcr<br />

mernber can help.<br />

I hope X can persuade more mernbers t1; repolt sightings of rcptile s and<br />

rrnphibio. I am sure therc must hre rnorc than one newt in North<br />

Yorkshire!<br />

If reporteC sightings Co incrcase ilcxt ye;ir (ptreasc make an effort!) it<br />

will nct mean that mrmbers of animals have necessari-ly increased but<br />

it wili be interesting to l1ote the hahitars of varicrus com"mon creiltures<br />

anri important to notc any disastcrs as weti as reccrding the existence<br />

of ;rny rarities.<br />

SUE EVANS

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