As a whole, 25 examples passed away a minumum of one regarding the selection criteria sets ( dining dining Table 2). The interpretations of some examples reveal ambiguous outcomes, although passing the choice criteria. For instance, test PI07‐06A (Figure 3e) losses 80% for the NRM in the 1st four demagnetization actions, 68.1 W s, leading to a paleointensity estimate of 185.9 ВµT. The demagnetization that is quick of test additionally the overprint regarding the NRM might suggest an impact of lightning even though other examples of this web site try not to show indications of lightning. Since this is the only test calculated with this website, the behavior can’t be when compared with other examples. Our microwave Thellier results highlight the importance of using web web site selection requirements towards the acquired sample that is individual. For the 10 internet web sites calculated from the microwave system, two web web internet sites, PI01 and PI16, passed the website selection requirements.

Examples from all internet web web sites had been put through the pseudo‐Thellier paleointensity experiment. Five to 11 specimens had been very first stepwise demagnetized using alternating fields as much as 270 mT (part 4). The exact same alternating industry actions and a bias field of 40 µT are acclimatized to give partial anhysteretic remanent magnetizations (pARMs). Finally, the acquired ARM ended up being demagnetized with the exact same industry steps to check on the linearity for the NRM‐demag vs. ARM‐demag. The info had been analyzed with paleointensity.org (Béguin et al., 2020 ). The auto‐interpretation function ended up being used in combination with a collection of selection requirements particularly created for pseudo‐Thellier experiments, pTh‐SCRIT (Béguin et al., 2020 ). The main focus of the set is from the linearity regarding the best‐fit lines in every three plots (Arai, ARM‐ARM, and Demag‐Demag plots) as well as on the choice associated with the remnant that is characteristic (ChRM), where all signs and symptoms of overprints regarding the NRM need to be eliminated to pass through the choice. Through the 146 calculated specimens, 65 specimens passed the B criteria that are 1/2ARM. Of which seven web web web sites hold realistic paleointensity estimates in line with the pTh‐SCRIT requirements set while the web web web site selection criteria (Figure 3 and dining dining Table 2).

6 Conversation

6.1 Paleodirections

6.2 Multimethod Paleointensity Data From Pico Island

Seventeen web internet web sites were afflicted by a couple of paleointensity approaches, of which 12 web sites passed away one or more regarding the protocols and matching test and web web web site data; for example., a niche site success rate of 70%. The 3 paleointensity techniques depend on comparing the NRM regarding the specimen having a magnetization that is laboratory‐induced the technique utilized to cause the laboratory magnetization is significantly diffent for every single regarding the practices. The persistence regarding the paleointensity results through the paleointensity that is multimethod can be viewed as dependability check ( ag e.g., Biggin & Paterson, 2014 ; Böhnel et al., 2009 ; de Groot et al., 2013 ; Monster et al., 2015 ). Site PI05 passed both pseudo‐Thellier and Thellier that is thermal paleointensity. Web Site PI16 passed all three paleointensity protocols. The obtained paleointensity estimates from the different protocols are outside each other’s confidence intervals in both cases. The consistency between different methods is low for these sites. The thermal Thellier outcomes of site PI16 is 24 µT higher than the acquired pseudo‐Thellier. The microwave oven Thellier result for web web web site PI16 (59.4 µT) is in‐between the pseudo‐Thellier and thermal Thellier consequence of 51.8 and 75.8 µT, correspondingly. For web site PI05, the result that is pseudo‐Thellier 10 µT more than the acquired thermal Thellier estimate. As all interpretations pass our selection requirements and therefore are theoretically similarly proper, it really is impractical to imply which method yields the estimate that is correct of paleofield. web web Sites with close ages, e.g., PI02 and PI13 or PI04 and PI07, reveal comparable paleointensity quotes, within mistake, acquired by different ways; the thermal Thellier outcome of PI02 (44.0 ± 6.1 µT) therefore the pseudo‐Thellier consequence of PI13 (41.9 ± 5.4 µT), additionally the pseudo‐Thellier outcome of PI04 (39.3 ± 2.2 µT) and also the thermal Thellier result of PI07 (43.2 ± 4.9 µT). This leads to a high persistence between the paleointensity estimates acquired from various protocols of these web internet internet sites.