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Table A1 LA-ICP-MS zircon U-Pb data of Laoniushan granitoids
The NWW-striking Qinling Orogen formed in the Triassic by collision between the North China and Yangtze Cratons. Triassic granitoid intrusions, mostly middle- to high-K,... -
Appendix 1. Single-zircon Pb evaporation ages from the Djupkilsodden granitoi...
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(Supplementary table 3) Start and end frequencies and duration of tonal call ...
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Experiment on marine fungus Microascus brevicaulis strain: Comparative growth...
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Scalloped hammerhead shark (Sphyrna lewini) tracking records in the Red Sea (...
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Nd and Sr isotopes of sediment core KL23 (M31/2-84_PC6)
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(Table 1) Diving behaviour of male Adélie penguins (Pygoscelis adeliae) with ...
The amount of energy that organisms can allocate to self-maintenance and/or reproduction largely depends on their foraging strategies. Because of corticosterone (CORT)... -
Foraminifera boron isotope, sea surface temperature, salinity, pH and pCO2 da...
Data presented here are trace-elements and boron isotope composition of planktic foraminifera G. ruber (250-355 μm) along with reconstructed surface ocean temperature, salinity,... -
Radiocarbon dating from DH-7B sediment core from the Dahu Lake, Ilan Plain
A 35-meter-long sediment core (DH-7B) was retrieved from Dahu Lake using a stainless-steel pipe mounted on a floating platform. The core was subsampled at 5-cm intervals with... -
(Table S4) Geochemistry of sediment core MD99-2254
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Experimental conditions for respiration and growth studies of F0 and F1 larva...
Water parameters in the 2 years before spawning of F0 (08.02.2016-06.03.2018) and during larval and juvenile phase of F1: Larval period until 17.05.2018 (48 dph, 900 dd) and...
