Sandelzhausen
Basic information
Sample name: Sandelzhausen
Reference: M. Böhme. 2010. Ectothermic vertebrates (Actinopterygii, Allocaudata, Urodela,
Anura, Crocodylia, Squamata) from the Miocene of Sandelzhausen (Germany, Bavaria) and their implications for environment reconstruction and palaeoclimate. Paläontol Z 84:3-41 [ER 4268]
Geography
Country: Germany
State: Bavaria
Coordinate: 48.628° N, 11.796° E
Latlng basis: stated in text
Scale: basin
Time interval: Early Miocene
Max Ma: 16.47
Min Ma: 16.27
Age basis: paleomag
Geography comments: "The Sandelzhausen locality (Fig. 1) is situated in the eastern part of the town of Mainburg, 70 km northeast of Munich and 27 km west of Landshut, in Lower Bavaria"
"Palaeomagnetic analysis of the Sandelzhausen profile reveal one inverse to normal magnetic reversal, which cannot unambiguously be correlated to the Global
Polarity Timescale (Abdul-Aziz et al. 2008). The palaeomagnetic results of other sections in the LandshutMainburg area, together with biostratigraphic information, makes a correlation to the magnetic reversals C5Cn.2r/2n
or C5Cn.1r/1n most reliable (Abdul-Aziz et al. 2008), placing Sandelzhausen at around 16.47 or 16.27 Ma, in
the latest Early Miocene, near the Early/Middle"
"Palaeomagnetic analysis of the Sandelzhausen profile reveal one inverse to normal magnetic reversal, which cannot unambiguously be correlated to the Global
Polarity Timescale (Abdul-Aziz et al. 2008). The palaeomagnetic results of other sections in the LandshutMainburg area, together with biostratigraphic information, makes a correlation to the magnetic reversals C5Cn.2r/2n
or C5Cn.1r/1n most reliable (Abdul-Aziz et al. 2008), placing Sandelzhausen at around 16.47 or 16.27 Ma, in
the latest Early Miocene, near the Early/Middle"
Environment
Lithology: siliciclastic (mixed)
Taphonomic context: fluvial deposit
Habitat comments: "a fine-clastic intercalation near the top of the regionally widespread sands and gravels of the No¨rdlicher Vollschotter"
"Fine to medium-sized gravels within a sandy to marly matrix. Pedogenic carbonate nodules and carbonatic cementations are very frequent"
"Fine to medium-sized gravels within a sandy to marly matrix. Pedogenic carbonate nodules and carbonatic cementations are very frequent"
Methods
Life forms: fishes, salamanders, frogs, other reptiles, lizards
Sample size: 4224 specimens
Museum: Bavarian State Collection for Palaeontology and Geology (BSPG)
Net or trap nights: 0
Basal area status: not applicable
Metadata
Sample no: 4658
Contributor no: John Alroy
Enterer: Nicholas Vine
Created: 2025-02-06 04:48:54
Modified: 2025-02-06 04:48:54
Abundance distribution
Each square represents a species. Square sizes are proportional to counts. Values are logged.
Statistics
37 species
4 singletons
total count 4224
geometric series index: 50.1
Fisher's α: 5.58
geometric series k: 0.8126
Hurlbert's PIE: 0.7463
Shannon's H: 1.8597
Good's u: 0.9991
Register
| Palaeocarassius sp. A | 1758 | |
| Palaeoleuciscus sp. A | 33 | |
| †Channa elliptica | 145 | |
| Gobius sp. | 3 | |
| †Albanerpeton inexpectatum | 8 | |
| †Salamandra sansaniensis | 95 | |
| Chelotriton sp. | 43 | |
| Triturus cf. vulgaris | 285 | |
| Triturus cf. marmoratus | 201 | |
| †Latonia gigantea | 54 | |
| †Pelobates fahlbuschi | 1079 | |
| Eopelobates sp. | 10 | |
| Bufo cf. viridis | 11 | |
| Bufo sp. | 1 | |
| Pelophylax sp. | 28 | |
| Ranidae indet. | 11 | |
| Diplocynodon styriacus | 331 | |
| Chamaeleo aff. caroliquarti | 5 | |
| Chamaeleo bavaricus | 4 | |
| Lacerta "s.l. sp. 1" | 1 | |
| Lacerta "s.l. sp. 2" | 9 | |
| Lacerta "s.l. sp. 3" | 21 | |
| Edlartetia sansaniensis | 1 | |
| Lacertidae cf. "Miolacerta tenuis" | 2 | |
| Tropidophorus bavaricus | 3 | |
| Scincidae indet. 1 | 2 | |
| Scincidae indet. 2 | 2 | |
| Bavaricordylus molassicus | 1 | |
| Bavaricordylus cf. molassicus | 6 | |
| Cordylidae indet. | 2 | |
| Scincomorpha indet. | 6 | |
| Pseudopus laurillardi | 18 | |
| Ophisaurus sp. | 30 | |
| Ophisaurus sp. I sensu | 8 | |
| Anguidae cf. "Ophisaurus cf. spinari" | 3 | |
| Anguidae indet. | 2 | |
| Palaeoblanus sp. | 2 | |