Tab.1. . MEERFELDER MAAR Drilling B 4
STRA TtGRAPHY and sequence of the lake sediments in 8 4
not visible layered mud
Chironomids
upper boundarv of varvite essentially littoral Taxa no indication of oligotrophy dominant: Tanytarsus
planctonic Cladoceras
(Daphnia, Bosmina)
high abundance Bosmma tong•rostrls
(missing or rare:
Daphnoat
littoral Cladoceras (Chydoridae)
Increase of the number of species,
no indication of oligotrophy dominant
rectangula
Glyptotend•pes Pleuro~us trlgonellus
Loss 01
' ~~
Microtend•oes D•crotendipes1 - - - ---jG""''''b'""''"''"''"l
Chydorus sphaerrcus)~' 01 """'f----C' _ "_"_"_"_'_--j Alonella eJugua
. - ORYAS3
ALLER6D
-
WEICHSEL HIGH GLACIAL PERIOD(?)
?
Increase of the number of species, essentially littoral
Taxa dominant Paratanytarsus Tanytarsus CriCOtopus Psectrocladius
Microtendipes
poor in species, high abundance 'subarctic'
Daphn•a dominant:
(missing or rare: Chydorus snhacncus Bosm•roa longorostr~s) Acropcrus harpae A Iona rectangula Alonella nana
poor in species dominant Chydorus sphaencus
A Iona rectangula
lleydo:::n:u:~';:~:utans
CRUSTACEANS OSTRACODES
autochthonous limnic
I I I
~
0
5
r
Drilling B 3
Core 13 (last core) total sample
T e r t i a r y F a u n a Cysts of
X X
XX
l·x •
X
X'x
a n d
X
F I o r a
Forami.nife.rs indet e.lett•ca mphiSYIICnSIS
f--
Hanzawa1a amph•SyhcnSISCyamocytheridea sp.
Lamellibranchs (Polymesoda ?)
Hemicypr1dC1S (Brst) Lamellibranchs Gastropods
I
{Eiph•d•um?non•onino•des Hemicyprode•s cf. basiliensis Lamellibranchs1---f--+-+- +---+--+-+-+----11---t--+-+-+---+- --lH'
!Hem•cy.proae•s !Brst) Balanus sp Lamelhbranchs Gastropodsi i (Brst.)
H ~amellibranchs
t---t- -+- + - +---+- -+-+- +----1---t- -+- + - +---+----1: L
Gastropods.
Hem1cypride1S (Brst) Lamellibranchs
Lamellibranchs
*Attention
Crosses indicate results.of a total sample of a core
Remark: additional fauna of Bolivina sp., Globigerinita sp. juv. in drilling 3, core 10. sample 13
Supplement to Negendank et al.
The Meerfelder Maar lake Deposits Zeitschrift fOr Gletscherkunde und Glazialgeologie
Vol. 21, 1985, p. 67-70
INTENSITY SUSCEPTIBILITY INCLINATION
INMA/M IN10-6St NAM
O 0 20 40 60 80 tOO 0 0 300 600 900 O oi-_3::.:0:___:.:60:..._.:_.90.
10
15
20
Tulf
DIATOM-VAAVITE
(probable annual layered Diatomgyttja)
Siii/Sandlayers
CLA YISH SILT resp. SIL TY CLAY, not visible or indistinctly layered: fresh bluish black·. later on reddish.
OIATOMGYTT JA
GRADED BEDDING.fine sand ... ~ clay
Layer of talus of slate/graywacke (detrital material)
RHYTHMITE: lnterbedding of coarse silt and clayish fine silt (2-S(IQ)mm]: partially deformed or contorted
clayish SILT without bedding. in some cases lamination
a boulder of devonian slate
") from core 7 upwards (upper one third)