The Littorina transgression in southeastern Sweden and its relation to mid-Holocene climate...
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Transcript of The Littorina transgression in southeastern Sweden and its relation to mid-Holocene climate...
The Littorina transgression in southeastern Sweden and its relation to
mid-Holocene climate variability
SHI-YONG YU
GeoBiosphere Science CentreDepartment of Geology/Quaternary
SciencesLund UniversitySölvegatan 12SE-223 62 LUND
Supervisors
P. Sandgren, B. E. Berglund and L. Barnekow
What are sea-level changes?
Sabadini, 2002
Sea level is the location where ocean water intercepts the land
Sea-level changes are the result of the complex feedback among the Earth’s different spheres at variable response time scales
Future sea-level rise: an enigma
Munk, 2002
Cabanes et al., 2001
Sea-level history over the last 100 years was well recorded by tide gauges (2 mm/yr). An acceleration was observed over the last decade (3 mm/yr). Other components involved in this complex pattern are unclear.
The best prophet of the future is the past
To give a credible scenario of future sea-level rise, go back to the past to look at sea level adaptations to climate changes under similar boundary conditions to the present.
The Littorina transgression: A best
analogue to the present sea-level rise
Warming climate (the mid-Holocene thermal maximum)
Soar of greenhouse gases (e.g. CO2, CH4) level
Absence of major continent ice sheets
The Littorina transgression (8500-3000 cal. BP) is a manifestation of Baltic Sea level rise in response to the pronounced drawdown of global ice volume
Littorina littorea Linné
The Littorina transgression - hypotheses and causes
Several minor transgression waves (the Danish-Swedish view)Caused by changing global ice volume and regional climate conditions
One main transgression (the Finnish view)Caused by the uniform eustatic rise of global sea level
R evised f rom H yvärinen, 1991
Climate changed, so did Baltic Sea level
Evidence from both ice cores and deep-sea sediments reveal that the North Atlantic area has experienced millennial-scale climate changes.
L L L L L L L
0 100 200 300 400
D istance (m )
E levation(m a.s.l.)
c lay tillL L L L L
10 410 10 190 cal. BP6570 6400 cal. BP
34 coring po in ts peat eo lian sand w ave w ashed pebb les
w ave w ashed sand
O LSÄNG (1978)
-4
-2
0
2
4
6
8
10
NW
SE
21 22 23
24
2526
27 28 2930
3132
3334
Beach ridge, Olsäng (Mikaelsson, 1978)
Beach ridges, Inlängan island (Photo: Berglund, 1964)
5
6
7
8
9
0 10 20 30 40 50 60 70 80 90 100 110
9.4 m
8.1 m
6.3 m
m
m abovesea leve l
N N E
0 10 20 30 40 50 60 70 80 905
6
7
8
9
m
9.5 m
m abovesea leve l
IN LÄ N G A N (1956)
A S P Ö (1956)
8 .2 m
6.8 m
N
S
S S W
Beach ridges on Inlängan and Aspö islands (Berglund, 1964)
Isolation lakes and lagoons: excellent benchmarks of past sea level
Dating the isolation/contact of the basins may provide a powerful constraint on relative sea-level changes
Smygen lagoon (Photo: Berglund, 2000)
BB
BA LT IC
S E A
Biskopsm åla
Sm y gen
56 10 '
56 0'
15 07 ' 15 08 '500 m0
-1.0
+0.5 +3.0
+0.9
+0.9
+2.2
+4.5
3.0BA LT IC
S E A
500 m0
56 10'
56 0' 14 53' 14 54 '
15 00 ' E
56 10 ' N
14 59 ' E 15 00 ' E
Lake
Färsks jön
B ruksviken
BALTIC
SEAE levation (m a .s .l.)
10 2515 205
0
15 05 'E
56 10 'N
+3.0 m
L a k e R y ss j ö n
+7.2 m
+4.5 m
BA LT IC S E A
a b
c d
Smygen: -1 m
Hunnemara: 3 m
Ryssjön: 4.5 m
Färsksjön: 7.2 m
(the highest lake containing brackish sediments in Blekinge)
Fieldwork (Photo: Berglund, 2000)
Co
rin
g Magnetic core scanning
Su
b-s
am
pli
ng
Pollen analysis
Diatom analysis
Macrofossilanalysis
Mineral magnetism
Carbon (LOI)
Geochemistry
AMS dating
Palaeoecologicalinterpretation
Flowchart of lab analyses
First order sea-level changes: Eustasy vs. isostasy
A big thaw of the Antarctic Ice Sheet
1st story
Coastal basins: Precise sea-level “index points”
L L L L LL L LL L L L L
Smygen-1.0 m
L L L L L
12.5
11.5
10.5
9.5
8.5
7.5
6.5
5.5
4.5
3.5
2.5
1.5
Dep
th b
elow
wat
er le
vel (
m)
2820 110
2920 95
3950 85
5645 85
4555 105
3090 105
6020 95
7310 100 7220 90
8475 95
8225 95 9650 95
L L L L LL L L L LL L LL L L L L
2935 80
4575 95
4850 90
4800 95
4875 90
5455 90
6415 90 7860 95
8220 110
9890 100
Hunnemara3.0 m
L L L
L L LL L L L L L L L L L L L L
2100 100
3200 90
4610 105 5575 105 6575 100 5805 95 6705 95 7245 90
9005 95
9565 120
Facies Facies Facies
SB
OB
SF
OF
SB
OB
SF
OF
SB
OB
SF
OF
L L LL L L
L L L L L
SB
OB
SF
OF
FaciesKalvöviken-2.0 m
4580 115
5315 100 6440 100 7445 90 7700 95 8005 100 8440 100 9650 100
Facies
6470 110
L L L L LL L L L L L L L L L
SB
OB
SF
OF
6570 110 7200 100 6810 100 7240 140 7480 150 7660 120 8230 150 8630 140 8810 160 8530 110
Sörevik-2.0 m
Ryssjön4.5 m
6.5
5.5
4.5
3.5
2.5
1.5
Dep
th b
elow
wat
er le
vel (
m)
L L L
L L LL L LS
BO
B
SF
OF
Färsksjön7.2 m
4830 100 5250 90 5705 80 6150 95 6695 105
L L LL L LL L L
L L L
SB
OB
SF
OF
3820 65
6640 70 6220 70
3950 60
6090 70
5040 65
Siretorp5.0 m
L L L L L L L L L L L L LL L L
SB
OB
SF
OF
Hallarums mosse4.7 m
4585 70 5040 855665 85 5945 75 6220 85 6395 125 6950 90 7105 90
L L L L L L L L L L 3145 65 3545 65 4170 75
SB
OB
SF
OF
Inlängans mosse5.0 m
4270 60 4470 80
5290 65 5430 65 5700 70 5930 70
Lithology key
Grey clay
Sand
Gyttja clay
Clayey gyttja
GyttjaFine-detritus gyttja Coarse-detritus gyttja
Peat
L L L L L
L L L L L
L L L L L
B
FaciesFaciesFaciesFacies
Sedimentary faciesOpen freshwater (OF)
Shallow freshwater (SF)
Shallow brackish-water (SB)
Open brackish-water (OB)
The Littorina transgression is caused by a continuous ice-volume-equivalent sea-level rise, interspersed with variable rates
2500 3500 4500 5500 6500 7500 8500
Age (cal. yr BP)
- 2
0
2
4
6
8
Bal
tic r
elat
ive
sea
leve
l (m
)
-30
-25
-20
-15
-10
-5
0
Far
-fie
ld r
elat
ive
sea
leve
l (m
)
Southeastern Sw eden
Barbados
N ew G uinea
Tahiti
1 m m yr -1
15 m m yr -1
3 m m yr -1
A changing ice volume?
6500 7000 7500 8000 8500
Age (ca l. yr BP)
-38
-37
-36
-35
-34
-33
18O
(‰
SM
OW
)
-40
-39
-38
-37
-36
18O
(‰
SM
OW
)
0
5
10
15
Rat
e (m
m y
r-1)
-1 .4
-1 .2
-1
-0 .8
18O
(‰
PD
B)
A
B
C
D
• Storegga tsunami (Andrén, 2001)?
• Slow down of crustal rebound?
• Laurentide floods (Tooley, 1989)?
A global meltwater pulse 8000 years ago
• Rapid depletion of seawater 18O
• A IRD spike in the South Atlantic (Hodell et al., 2001)
• Flooding in Chesapeake Bay/8000 cal. BP (Bratton et al., 2003)
• A break of coral growth in the Caribbean area (Blanchon and Shaw, 1995)
• Black Sea transgression
Global climate during the “Noah’s Flood”
Linking Baltic Sea-level fluctuations to North Atlantic storminess at millennial time scale
Coastal dune, W Denmark (Photo: Yu, 2003)
2nd story
Dating sea-level-sensitive floras (e.g. dinoflagellates, diatoms, seagrasses, stoneworts) provides evidence for millennial-scale sea-level changes
9000 8000 7000 6000 5000 4000 3000 2000 1000 0
Age (ca l. BP )
-2 .0
0 .0
2 .0
4 .0
6 .0
8 .0
Rel
ativ
e se
a le
vel (
m)
-35 .4
-35 .2
-35
-34.8
-34 .6
-34 .4
18O
(‰
SM
OW
)
S örev ikK a lvöviken
S m ygen
H unnem ara
R yss jönS ire to rp
Färsks jönO lsäng
1. N W England2. W N etherlands
S torm surges
B each ridges3. N E Ire land4. Svalbard5. W M ed ite rranean
S and dunes
6. N S co tland7. W S cotland8. SW France9. W Ire land
10 . W D enm ark11 . N W E ngland12 . S W France13 . N W France14 . N W D enm ark15 . W D enm ark16 . N Fennoscandia
Ö ppenskär
U tlängan
17 . G reen land ice coreS ea-sa lt ions
Ble
king
ese
a-le
vel h
ighs
tan
dsN
ort
hG
RIP
ice
core
a
b
c
L1
L2L3
L4 L5
Centennial-scale sea-level changes: A window to the NAO past?
3rd story
0 1 2 3 4 5
O. centrocarpum( 103 cysts cm -2 yr-1)
2 4 6 8
GISP2 sea salt Na+
(p.p.b.)
6 8 10 12 14 16
Organic carbon(%)
10 100ARM
( 10-5 m3 kg-1)
2500
3500
4500
5500
6500
7500
8500
Age
(cal
. BP
)
0 0.1 0.2 0.3
Spinif er ites. spp.( 103 cysts cm -2 yr-1)
Regional transgression
A B C D E
L2
L3
L4
L5
Sea-level changes: Cycle, cycle all the time?
Per
iod
(yr)
128
256
512
1024
0 0.04 0.08 0.12
Pow er
180 yr
220 yr
480 yr
940 yr
1470 yr
95% c. l.A B0 0 .5 1 .0 2 .0 3 .0
Pow er (re la tive to g lobal)
3500 4500 5500 6500 7500
Age (cal. yr B .P .)
Wavelet and power spectral transforms of a macrofossil series from Lake Ryssjön
The 480-yr cycle:
tidal origin?
480*2=960 yr
480*3=1440 yr
the enigmatic 1500 yr cycle was solved!
Conclusions
•Within the Littorina Sea phase, five minor transgressions are recorded: L1 8500–8200, L2 7800–6900, L3 6400–5600, L4 5300–4700, and L5 4500–4100 cal. BP. These minor transgressions, lasting 500–1000 years in the study sites, occurred almost synchronously across the southern Baltic Sea.
•The Littorina transgression in southeastern Sweden covers the time span 8500–3000 cal. BP. It can be ascribed to the accelerated rise of global sea level, overprinting the slow isostatic uplift in southern Scandinavia during the middle Holocene.
•The first transgression (L1) can be linked to the flood of the proglacial lakes in North America. The most pronounced transgression (L2) is marked by a Baltic Sea level rise by ca. 8 m in 500 years, at an accelerated rate of ~15 mm yr-1. It suggests a global meltwater pulse probably triggered by the partial
collapse of the Antarctic Ice Sheet.
•The younger minor transgressions were possibly caused by ice-volume changes in combination with submillennial-scale variations in regional storminess.
•Centennial-scale sea-level fluctuations show good coherence with ice-core sea-salt ions and cosmogenic nuclides in some time windows, suggesting solar forcing probably through a system similar to the dipole oscillation of the North Atlantic atmosphere (i.e. NAO). In addition, tidal actions related to lunar cycles may exert another important influence on Baltic Sea level during the middle Holocene.