2
times, when Marsupiocrinus and Gissocrinus were common reef animals. TRILOBITES are probably the most famous fossil found on Wren’s Nest. Calymene (e) was so commonly found by the quarrymen in the 19th century that it became known as the “Dudley Locust” or the ‘Dudley Bug’ and was incorporated into the town’s coat-of- arms as a symbol of the limestone mining industry. Another common trilobite is Dalmanites (f). Trilobites were arthropods, related to modern crabs and lobsters, but they lacked the claws and special mouthparts of their carnivorous relatives and probably grazed on plants for food. Whole fossil trilobites are rarely found. The animals had to moult in order to grow, shedding their outer skin or exoskeleton in pieces. Most trilobite fossils are therefore of moulted exoskeletons and not of dead animals. Some of the easiest fossils to find on Wren’s Nest are BRACHIOPODS, such as Atrypa (g), Strophonella (h) and Leptaena (i). These are often confused with BIVALVES, like Goniophora (j) and Pteronitella (k), which were much rarer. The most obvious difference between the two types of fossil is that bivalves have valves or shells which are identical whereas brachiopods’ valves are of different sizes. Today bivalves are far more common than brachiopods. Other animals that lived on the reef included GASTROPODS (sea snails) like Poleumita (l) and Acroculia (m). Gastropods were probably vegetarian, but there were predatory animals on the reef as well. ORTHOCERAS (n) were relatives of modern day squids and cuttlefish. They had cone-shaped shells which could be several metres long and they were probably carnivores, using the long tentacles surrounding the head to catch smaller animals. Another predatory creature on the reef was the EURYPTERID or sea-scorpion (o). Eurypterids were arthropods, like trilobites, but they were much larger, growing up to 2 metres long and had claws for catching prey. Quarrying at Wren’s Nest The limestone rocks at Wren’s Nest have been exploited by man for hundreds of years. Originally the rock was used as a local building stone and it can be seen in the walls of Dudley Castle and Dudley Priory. Later it was discovered that burnt limestone, or lime, was a good fertiliser and the demand for the rock increased. Lime was produced by placing alternate layers of limestone and coal in a kiln and burning it for GEOLOGY Wren’s Nest was declared a National Nature Reserve in 1956, the first to be designated for its outstanding geology and we celebrate its 50th anniversary in 2006. Wren’s Nest is of international importance both for the quality and quantity of its fossils, but also for its value as an educational resource. Wren’s Nest Hill and Mons Hill are made of Wenlock limestone composed of the remains of ancient sea creatures that lived more than 400 million years ago. This period of geological time is known as the Silurian. These ancient fossils are so beautifully preserved that they are displayed in museums throughout the world and geologists come from far and near to study and collect them. Many of the best fossils were found in the 18th and 19th centuries. During this time the limestone rock was being excavated and burnt to produce lime, an important material for agriculture and industry. This mining activity left great scars on the flanks of the hill and many large and spectacular caverns. The Silurian World The Dudley area would have looked very different during Silurian times. Shallow seas covered the Midlands and the nearest land lay many miles to the east of Wren’s Nest. Plants were just beginning to colonise the land, but the seas were full of life, some of which would seem familiar to us today. At Wren’s Nest small coral reefs grew up providing a home for thousands of animals and plants, many of which have been preserved as fossils within the limestone. Some of the most common fossil animals to be found here are illustrated (right). There were many types of CORALS in the reef, Favosites (a) and Halysites (b) were compound types where many tiny coral animals (polyps) lived together; solitary corals like Dokophyllum (c) were less common. CRINOIDS grew in sheltered areas behind the main reef, in patches of sand or soft sediment. They are often called “Sea Lilies” because they look so much like plants, with roots, a stem and a flower-like ‘cup’ on top, but they were actually animals and are related to starfish and sea-urchins. Crinoids (d) still live in the seas today but are rarer than they were in Silurian The Geology of the Dudley Metropolitan Borough Council wishes to acknowledge the financial support of English Nature Background: Reef Limestone several days. The lime powder was then raked out from the bottom of the kiln. Several of these kilns can still be seen on the west side of the Nature Reserve. In the early 18th century a method was found to smelt iron using coal, so limestone, which was used as a flux in this process, became a valuable commodity. At first only surface outcrops of limestone were quarried, but soon the quarrymen began to dig underground to get to the purest and most valuable deposits. By the start of the 19th century, the mines and caverns extended so deep that it was too difficult to haul the rock to the surface; thus a system of underground canals was built so that the limestone could be carried away by barge to furnaces elsewhere in the Black Country. Background: Halysites Reef Limestone Seven Sisters cavern circa 2000 WREN’S NEST National Nature Reserve Fossilised exoskeleton of a Dalmanites trilobite Poleumita, a fossil sea-snail or gastropod Halysites, a compound coral Sagenocrinus a common Silurian crinoid Marsupiocrinus with roots still attached to the stem Calymene blumenbachii, the ‘Dudley bug’ Strophonella strophonella a common brachiopod Typical Silurian brachiopods Leptaena depressa Atrypa reticularis n b c e g f i j k l m d o a h

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Page 1: New The Geology of theWREN’S NEST TRILOBITES National Nature … · 2016. 3. 26. · TRILOBITES are probably the most famous fossil found on Wren’s Nest. Calymene (e) was so commonly

times, when Marsupiocrinus and Gissocrinus werecommon reef animals.

TRILOBITES are probably the most famous fossilfound on Wren’s Nest. Calymene (e) was so commonlyfound by the quarrymen in the 19th century that itbecame known as the “Dudley Locust” or the ‘DudleyBug’ and was incorporated into the town’s coat-of-arms as a symbol of the limestone mining industry.Another common trilobite is Dalmanites (f). Trilobiteswere arthropods, related to modern crabs and lobsters,but they lacked the claws and special mouthparts oftheir carnivorous relatives and probably grazed onplants for food. Whole fossil trilobites are rarely found.The animals had to moult in order to grow, sheddingtheir outer skin or exoskeleton in pieces. Most trilobitefossils are therefore of moulted exoskeletons and not ofdead animals.Some of the easiest fossils to find on Wren’s Nest areBRACHIOPODS, such as Atrypa (g), Strophonella (h)and Leptaena (i). These are often confused withBIVALVES, like Goniophora (j) and Pteronitella (k),which were much rarer. The most obvious differencebetween the two types of fossil is that bivalves havevalves or shells which are identical whereasbrachiopods’ valves are of different sizes. Todaybivalves are far more common than brachiopods.Other animals that lived on the reef includedGASTROPODS (sea snails) like Poleumita (l) andAcroculia (m). Gastropods were probably vegetarian,but there were predatory animals on the reef as well.ORTHOCERAS (n) were relatives of modern daysquids and cuttlefish. They had cone-shaped shellswhich could be several metres long and they wereprobably carnivores, using the long tentaclessurrounding the head to catch smaller animals.Another predatory creature on the reef was theEURYPTERID or sea-scorpion (o). Eurypterids werearthropods, like trilobites, but they were much larger,growing up to 2 metres long and had claws for catchingprey.

Quarrying at Wren’s Nest

The limestone rocks at Wren’s Nest have beenexploited by man for hundreds of years. Originally therock was used as a local building stone and it can beseen in the walls of Dudley Castle and Dudley Priory.Later it was discovered that burnt limestone, or lime,was a good fertiliser and the demand for the rockincreased. Lime was produced by placing alternatelayers of limestone and coal in a kiln and burning it for

GEOLOGY

Wren’s Nest was declared a National Nature Reserve in1956, the first to be designated for its outstandinggeology and we celebrate its 50th anniversary in 2006.Wren’s Nest is of international importance both for thequality and quantity of its fossils, but also for its valueas an educational resource. Wren’s Nest Hill and MonsHill are made of Wenlock limestone composed of theremains of ancient sea creatures that lived more than400 million years ago. This period of geological time isknown as the Silurian. These ancient fossils are sobeautifully preserved that they are displayed inmuseums throughout the world and geologists comefrom far and near to study and collect them.

Many of the best fossils were found in the 18th and19th centuries. During this time the limestone rock wasbeing excavated and burnt to produce lime, animportant material for agriculture and industry. Thismining activity left great scars on the flanks of the hilland many large and spectacular caverns.

The Silurian World

The Dudley area would have looked very differentduring Silurian times. Shallow seas covered theMidlands and the nearest land lay many miles to theeast of Wren’s Nest. Plants were just beginning tocolonise the land, but the seas were full of life, some ofwhich would seem familiar to us today. At Wren’s Nest

small coral reefs grew upproviding a home forthousands of animals andplants, many of whichhave been preserved asfossils within thelimestone. Some of themost common fossilanimals to be found hereare illustrated (right).

There were many types of CORALS in the reef,Favosites (a) and Halysites (b) were compound typeswhere many tiny coral animals (polyps) lived together;solitary corals like Dokophyllum (c) were less common.

CRINOIDS grew in sheltered areas behind the mainreef, in patches of sand or soft sediment. They are oftencalled “Sea Lilies” because they look so much likeplants, with roots, a stem and a flower-like ‘cup’ on top,but they were actually animals and are related tostarfish and sea-urchins. Crinoids (d) still live in theseas today but are rarer than they were in Silurian

The Geology of the

Dudley Metropolitan Borough Council wishes toacknowledge the financial support of English Nature

Background: Reef Limestone

several days. The lime powder was then raked out fromthe bottom of the kiln. Several of these kilns can still beseen on the west side of the Nature Reserve. In theearly 18th century a method was found to smelt ironusing coal, so limestone, which was used as a flux inthis process, became a valuable commodity.

At first only surface outcrops of limestone werequarried, but soon the quarrymen began to digunderground to get to the purest and most valuabledeposits. By the start of the 19th century, the minesand caverns extended so deep that it was too difficultto haul the rock to the surface; thus a system ofunderground canals was built so that the limestonecould be carried away by barge to furnaces elsewherein the Black Country.

Background: Halysites

Reef Limestone

Seven Sisters cavern circa 2000

WREN’S NESTNational Nature Reserve

Fossilised exoskeletonof a Dalmanites trilobite

Poleumita, a fossil sea-snail or gastropod

Halysites, a compound coral

Sagenocrinusa commonSiluriancrinoid

Marsupiocrinuswith roots still

attached to thestem

Calymene blumenbachii,the ‘Dudley bug’

Strophonella strophonellaa common brachiopod

Typical Silurian brachiopods

Leptaena depressa

Atrypa reticularis

n

b

ce

gf

ij

kl

m d

o

a

h

Page 2: New The Geology of theWREN’S NEST TRILOBITES National Nature … · 2016. 3. 26. · TRILOBITES are probably the most famous fossil found on Wren’s Nest. Calymene (e) was so commonly

WREN’S NESTNational

Nature Reserve

WARDEN’SOFFICE

A457 SEDGLEY ROAD

A4123 BIRMINGHAM NEW ROAD

A4168 PRIORY RD

WREN’S HILL ROAD

PARKES HALL

ROAD

LINWOOD RD

To WOLVERHAMPTON

To DUDLEY CARPARK

BluebellPark

MAYFIELD

RDBLUEBELL ROAD

ToBIRMINGHAM

SC

ALE

(Metres)

0 100

200

WA

RD

EN

’SO

FF

ICE

MO

NS

HILL

Wood

setton Method

ist Church

Green P

ool

Farm

Parkes H

allR

oad

Wren’s N

estR

oad

Hillsid

eR

oad‘The C

aves’P

ublic H

ouseCaves

PoolC

ollegeB

uildings

View

ofQ

uarry

View

ofQ

uarry

Wren’s H

illR

oad

View

ingP

latformR

ipp

le Bed

s

The Quarry

Lime K

ilns

Seven

Sisters

CavernC

herryH

ole

Ninety-nine

Step

sM

eadow

Road

Myrtle

Road

Ced

arR

oad

WR

EN

’S N

ES

TH

ILL

Wren’s H

illR

oad

Linwood

Road

Mayfield

Road

Blueb

ell Park

Blueb

ell Road

Lime P

yes

FieldField

Field

Fo

ssil Co

llecting C

od

e

1.For your ow

n safety please

DO

NO

Tclim

b on the rock

exposures. R

ock faces can be

unstable and

dangerous.

2.The use of ham

mers or other

tools on the reserve is ST

RIC

TLY

P

RO

HIB

ITE

D.

Never collect

fossils directly from

rock faces.

3.Fossils m

ay be collected

from the

loose material at the b

ase of slop

es. Please only take aw

ay a few

small rep

resentative samp

les.

4.For help

with id

entification please

contact the Ward

en Service on

01384 812785 or Dud

ley Museum

on 01384 815575. R

emem

ber to

keep a note of the exact location

your fossil was found

.

5.If you no longer w

ish to keep your

fossils, remem

ber never throw

them

away! D

onate them to the

Museum

or the Ward

en Service

for others to enjoy.

THA

NK

YO

U

1

2

3

4

5

6

7

7

11

8

9

10

KE

YG

eological trail markers

- see separate field

guide

View

point

Footpaths

Step

s

Security Fence

Reserve B

oundary

The Geology of theWREN’S NESTNational Nature Reserve

As the quarrymen worked they found many wonderfulfossils. These were purchased by dealers, to be soldthrough local fossil shops. No doubt the vastmajority must have been lost forever in the furnaces ofthe ironworks.By the early 20th century there was much less demandfor Wren’s Nest limestone and by 1924 it was no longerprofitable to mine and the quarries were closed. Todayall the former underground workings are closed to thepublic. It is however, still possible for groups to view theoriginal ‘Seven Sisters’ by prior arrangement with thewarden service. Please phone for details. The SevenSisters are massive rock pillars that once supported theroof of a vast cavern complex descending 100 metresbelow the ground. Only five pillars of the original sevennow remain.In 1973 the Dudley Canal Trust opened up part of theunderground canal network beneath nearby Castle Hilland narrowboat trips are now run from the BlackCountry Museum into the famous Singing Cavern.Here an exciting audio-visual show re-creates life in alimestone mine.

Safety InformationRock exposures can be unstable and visitors arerequested to exercise care and caution when visitingthe reserve. Due to essential engineering works it hasbeen necessary to extend the safety fencing and re-route certain paths. We apologise for anyinconvenience this may cause. Please remain ondesignated paths and observe any path closures ordiversions. It is strictly prohibited to enter the areasinside the safety fences.Visitors to the Reserve do so entirely at their own risk.Neither Dudley Metropolitan Borough Council orEnglish Nature can accept liability or responsibility forloss, damage or injury to property or, in absence ofnegligence, to persons.

Other publications availableThe Wildlife of Wren’s Nest National Nature ReserveWren’s Nest National Nature Reserve GeologicalHandbook and Field Guide

Wren’s Nest Warden ServiceThe nature reserve has a team of three full timewardens who maintain and care for the site’s geologicalfeatures and wildlife. We always welcome help fromvolunteers. For more information on volunteering or tobook a school visit, guided walk or illustrated talkplease contact 01384 812785.

Dudley Museum & Art GalleryTo complement your trip to Wren’s Nest pay a visit tothe Museum & Art Gallery. Here there is an extensivegeological collection and fine displays of fossils fromWren’s Nest and the local coal measures. Staff areavailable on weekdays to offer general advice ongeology. Books, fossil replicas, posters, postcards etc.are available in the Museum shop. ADMISSION FREE.Dudley Museum & Art Gallery, St. James’s Road,Dudley, West Midlands DYl 1 HUContact - The Keeper of Geology Tel. (01384) 815575.

Geological SocietiesThe Black Country Geological Society is made up ofboth professional and amateur geologists. Meetings areheld at the Ward Arms and Dudley Museum in Dudley.The society arranges talks and field trips. For moreinformation contact the society at www.bcgs.info

Background: Flower meadow at Wren’s Nest National NatureReserve.

View of the Quarry

The Ripple Beds

www.dudley.gov.uk

WREN’S NEST

WREN’S NEST

National Nature Rese

rveN

ational Nature Reserv

e