<|begin_of_text|><|start_header_id|>system<|end_header_id|>You are an expert on climate change, human mobility and migration. Answer the question truthfully.<|eot_id|><|start_header_id|>user<|end_header_id|>Here are the title and abstract of a scientific paper probably related to climate change, human mobility and migration..
Title:"Taphonomic and paleoecological aspects of large mammals from Sudety Mts (Silesia, SW Poland), with particular interest to the carnivores."
Abstract:"The rediscovery of old collections and revision of the fossil material from more than 30 Sudeten caves and rock shelters allow reconstructing the faunal changes during the Late Pleistocene and the Holocene. We found that the composition of mammalian assemblages of Sudety Mts during MIS 3 differed significantly from the Holocene and modern one, and reflected the colder climate. Mammals belonging to the Mammuthus-Coelodonta faunal complex inhabited open flattened lowlands (Bohemia, Moravia and Silesia) surrounding Sudeten area. Several large carnivores (Canis lupus spelaeus, Ursus arctos priscus, Ursus ingressus, Gulo gulo, Mustela eversmanii, Panthera spelaea spelaea, Crocuta crocuta spelaea) as well as herbivores (Mammuthus primigenius, Coleodonta antiquitatis, Megaloceros giganteus, Rangifer tarandus, large form of Equus ferns, Bison priscus, and Ovibos moschatus) made up the core of this assemblage. Our studies showed that most of these faunal elements were also present in Sudety Mts, despite the previous opinion that these mountains formed an effective natural barrier during the Late Pleistocene. Besides, it seems that during cold phases they could be refugees for forest animals, which were also present in the Mammuthus-Coelodonta faunal complex, but lower quantities. They avoided flat treeless Silesian lowlands and concentrated in mountainous and hilly regions. In this context, during the Late Pleistocene Sudety Mts were a forested island confined to elevated areas or river valleys. Range extensions, contractions, and continuations on different scales resulted in mammalian paleoassemblages which differed in particular from the modern ones. The analysis of the mammal faunas from Sudeten sites revealed that there were three heterochronous mammalian faunal complexes replaced each other throughout the Late Pleistocene and the Holocene. Differences between these assemblages resulted from changes in morphology, areas and extinction of several species. The existence of different faunal elements was distinguished by the chronological and geographical change in the structure of mammalian assemblages. At the end of MIS 3 most of the cold-adapted species from the Mammuthus-Coelodonta faunal complex like Ursus ingressus, Panthera spelaea spelaea, Coelodonta antiquitatis, Bison priscus, and Megaloceros giganteus disappeared. During the second phase, at the latest Pleistocene and the Holocene boundary, all the species of the Mammuthus-Coelodonta faunal complex still not became extinct. Several species from this assemblage disappeared later in the Holocene. It should be noted that the role of the human in the changes of faunal complexes and species extinctions during the Late Pleistocene and the Holocene in the Sudety Mts cannot be so far demonstrated.."
I have six questions you need to answer.
Q1: Is this article is about 'human migration mobility': 1 = yes; 0 = no. Answer with a number. Do not give a textual explanation.

Q2: What drivers of migration and mobility does the article study? 0 = 'other', 1 = 'climate', 2 = 'environment', 3 = 'economic', 4 = 'conflict', 5 = 'political', 6 = 'social', 7 = 'family'. Answer with a number or a sequence of numbers separated by commas. Do not give a textual explanation. 

Q3: What is the overall sentiment of the article?:0 = 'neutral', 1 = 'negative', 2 = 'positive'. Answer with a number. Do not give a textual explanation.

Q4: What type of climate or environmental keywords are explicitly mentioned?:  0 = 'none', 1 = 'algal blooms', 2 = 'infestation', 3 = 'infectious diseases', 4 = 'ocean acidification', 5 = 'sea ice', 6 = 'acid rain', 7 = 'drought', 8 = 'cold wave', 9 = 'heat wave', 10 = 'glacial', 11 = 'wildfire', 12 = 'air pollution', 13 = 'biodiversity loss', 14 = 'coastal erosion', 15 = 'land degradation', 16 = 'deforestation', 17 = 'desertification', 18 = 'water pollution', 19 = 'diebacks', 20 = 'permafrost loss', 21 = 'sand mining', 22 = 'sea level rise', 23 = 'earthquake', 24 = 'tsunami', 25 = 'volcanic', 26 = 'flood', 27 = 'avalanche', 28 = 'landslide', 29 = 'downburst', 30 = 'thunderstorm', 31 = 'sandstorm', 32 = 'haze', 33 = 'storm', 34 = 'cyclone', 35 = 'blizzard', 36 = 'hail', 37 = 'snow', 38 = 'tornado', 39 = 'wind', 40 = 'hurricane', 41 = 'typhoon', 42 = 'other'. Answer with a number or a sequence of numbers separated by commas. Do not give a textual explanation. 

Q5: What discipline does the article belong to?: 0 = 'other', 1 = 'social science', 2 = 'natural science', 3 = 'arts and humanities', 4 = 'multidiscipline and interdiscipline'. Answer with a number. Do not give a textual explanation.

Q6: Does the article apply quantitative and/or statistical analysis?: 0 = 'no', 1 = 'yes'. Answer with a number. Do not give a textual explanation.

Use the following template: 

Q1 = [];
Q2 = [];
Q3 = [];
Q4 = [];
Q5 = [];
Q6 = [].<|eot_id|><|start_header_id|>assistant<|end_header_id|>Answer:
Q1 = [0];
Q2 = [];
Q3 = [];
Q4 = [];
Q5 = [];
Q6 = [1].
Taphonomic and paleoecological aspects of large mammals from Sudety Mts (Silesia, SW Poland), with particular interest to the carnivores
The rediscovery of old collections and revision of the fossil material from more than 30 Sudeten caves and rock shelters allow reconstructing the faunal changes during the Late Pleistocene and the Holocene. We found that the composition of mammalian assemblages of Sudety Mts during MIS 3 differed significantly from the Holocene and modern one, and reflected the colder climate. Mammals belonging to the Mammuthus-Coelodonta faunal complex inhabited open flattened lowlands (Bohemia, Moravia and Silesia) surrounding Sudeten area. Several large carnivores (Canis lupus spelaeus, Ursus arctos priscus, Ursus ingressus, Gulo gulo, Mustela eversmanii, Panthera spelaea spelaea, Crocuta crocuta spelaea) as well as herbivores (Mammuthus primigenius, Coleodonta antiquitatis, Megaloceros giganteus, Rangifer tarandus, large form of Equus ferns, Bison priscus, and Ovibos moschatus) made up the core of this assemblage. Our studies showed that most of these faunal elements were also present in Sudety Mts, despite the previous opinion that these mountains formed an effective natural barrier during the Late Pleistocene. Besides, it seems that during cold phases they could be refugees for forest animals, which were also present in the Mammuthus-Coelodonta faunal complex, but lower quantities. They avoided flat treeless Silesian lowlands and concentrated in mountainous and hilly regions. In this context, during the Late Pleistocene Sudety Mts were a forested island confined to elevated areas or river valleys. Range extensions, contractions, and continuations on different scales resulted in mammalian paleoassemblages which differed in particular from the modern ones. The analysis of the mammal faunas from Sudeten sites revealed that there were three heterochronous mammalian faunal complexes replaced each other throughout the Late Pleistocene and the Holocene. Differences between these assemblages resulted from changes in morphology, areas and extinction of several species. The existence of different faunal elements was distinguished by the chronological and geographical change in the structure of mammalian assemblages. At the end of MIS 3 most of the cold-adapted species from the Mammuthus-Coelodonta faunal complex like Ursus ingressus, Panthera spelaea spelaea, Coelodonta antiquitatis, Bison priscus, and Megaloceros giganteus disappeared. During the second phase, at the latest Pleistocene and the Holocene boundary, all the species of the Mammuthus-Coelodonta faunal complex still not became extinct. Several species from this assemblage disappeared later in the Holocene. It should be noted that the role of the human in the changes of faunal complexes and species extinctions during the Late Pleistocene and the Holocene in the Sudety Mts cannot be so far demonstrated.